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Mississippi Valley Division Engineer Research and Development Center Pictorial Account and Landscape Evolution of the Crevasses near Fort St. Philip, Louisiana MRG&P Report No. 2 • January 2014

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Page 1: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

Mississippi Valley Division Engineer Research and Development Center

Pictorial Account and Landscape Evolution of the Crevasses near

Fort St. Philip, Louisiana MRG&P Report No. 2 • January 2014

Page 2: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

Mississippi River Geomorphology and Potamology Program

MRG&P Report No. 2 January 2014

Pictorial Account and Landscape Evolution of the Crevasses near Fort St. Philip, Louisiana

Glenn M. Suir Environmental Laboratory U.S. Army Engineer Research and Development Center Wetlands and Environmental Technologies Research Facility Louisiana State University - Wetland Resources Building Baton Rouge, LA 70803

William R. Jones U.S. Geological Survey (USGS) National Wetlands Research Center 700 Cajundome Boulevard Lafayette, LA 70506

Adrienne L. Garber Five Rivers Services, LLC National Wetlands Research Center 700 Cajundome Boulevard Lafayette, LA 70506

John A. Barras U.S. Geological Survey (USGS) Coastal and Marine Science Center 600 Fourth Street South St. Petersburg, FL 33701

Final report Approved for public release; distribution is unlimited.

Page 3: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MRG&P Report No. 2 ii

Abstract

Quantifying the effects of active natural and constructed crevasses is critical to the planning and success of future ecosystem restoration activities. This document provides a historical overview of landscape changes within the vicinity of the natural crevasses near Fort St. Philip, Louisiana. A significant event influencing landscape change within the Fort St. Philip study area was the breaching of the eastern levee of the Mississippi River. Initially, the river water that was diverted through these crevasse channels physically removed significant marsh areas within the study area. These initial direct impacts were succeeded by several decades of larger regional loss patterns driven by subsidence and other episodic events (e.g, hurricanes and floods), and recent localized land gains. These increases in land area are potentially the long-term results of the Fort St. Philip crevasses, and the short-term impacts of delta management activities. However, for the majority of the 1956-2008 period of analysis, the crevassing of the eastern bank of the Mississippi River levee was a loss accelerant in the Fort St. Philip area.

DISCLAIMER: The contents of this report are not to be used for advertising, publication, or promotional purposes. Citation of trade names does not constitute an official endorsement or approval of the use of such commercial products. All product names and trademarks cited are the property of their respective owners. The findings of this report are not to be construed as an official Department of the Army position unless so designated by other authorized documents. DESTROY THIS REPORT WHEN NO LONGER NEEDED. DO NOT RETURN IT TO THE ORIGINATOR.

Page 4: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MRG&P Report No. 2 iii

Contents Abstract .......................................................................................................................................................... ii

Figures and Tables ........................................................................................................................................ iv

Summary ......................................................................................................................................................... vi

Preface ...........................................................................................................................................................vii

Unit Conversion Factors ........................................................................................................................... viii

1 Introduction ............................................................................................................................................ 1 1.1 Background .................................................................................................................... 1 1.2 Purpose .......................................................................................................................... 1 1.3 Project area .................................................................................................................... 3

2 Methods .................................................................................................................................................. 4 2.1 Data acquisition and processing .................................................................................. 4 2.2 High-resolution data ...................................................................................................... 6 2.3 Moderate-resolution data ............................................................................................. 7

3 Results .................................................................................................................................................... 8 3.1 Aerial photography ......................................................................................................... 8 3.2 Landscape area and change – High-resolution analyses ......................................... 10 3.3 Landscape area and change – Moderate-resolution analyses ................................. 31

4 Conclusions .......................................................................................................................................... 34

References ................................................................................................................................................... 35

Report Documentation Page

Page 5: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MRG&P Report No. 2 iv

Figures and Tables

Figures

Figure 1. Fort St. Philip Crevasses study location map. ............................................................................ 2 Figure 2. Daily Mississippi River stage data (water level, in feet) at Empire gage (blue) and Venice gage (green), Louisiana. Flood stage peak identified with red circle. ........................................ 8 Figure 3. Aerial photography showing pre- (left pane), active- (middle pane), and post-breaching (right pane) of the Mississippi River levee near Fort St. Philip, Louisiana in 1970, 1973 (moderate-resolution photography experiencing Moiré effect), and 1974, respectively. Breach site identified with red ovals. .................................................................................... 9 Figure 4. Fort St. Philip study area - 1956 high-resolution photomosaic map. ................................... 11 Figure 5. Fort St. Philip study area with access canals (#1) - 1970 high-resolution photomosaic map (Table 2). ....................................................................................................................... 12 Figure 6. Fort St. Philip study area with crevasse locations (#2), areas with major land-to-water conversion (#3), and formation of crevasse channels (#4) - 1978 high-resolution photomosaic map (Table 2). ....................................................................................................................... 13 Figure 7. Fort St. Philip study area with areas of land-to-water conversion (#3), crevasse channel development (#4), and large impoundment area (#5) - 1989 high-resolution photomosaic map (Table 2). ....................................................................................................................... 14 Figure 8. Fort St. Philip study area with areas of land-to-water conversion (#3), crevasse channel development (#4), and large impoundment area (#5) - 1998 high-resolution photomosaic map (Table 2). ....................................................................................................................... 15 Figure 9. Fort St. Philip study area constructed Coastal Wetlands Planning, Protection, and Restoration Act BS-11 project terraces (#6) - 2008 high-resolution photomosaic map (Table 2). ........................................................................................................................................................ 16 Figure 10. Delta Management at Fort St. Philip project area - 2011 high-resolution photomosaic map (USFWS 2013b). .......................................................................................................... 17 Figure 11. Fort St. Philip study area - 1956 high-resolution land-water classification map. ............. 19 Figure 12. Fort St. Philip study area - 1970 high-resolution land-water classification map. ............. 20 Figure 13. Fort St. Philip study area - 1956-1970 high-resolution land change analysis map. ............ 21 Figure 14. Fort St. Philip study area - 1978 high-resolution land-water classification map. .................. 22 Figure 15. Fort St. Philip study area - 1970-1978 high-resolution land change analysis map. ............. 23 Figure 16. Fort St. Philip study area - 1988 high-resolution land-water classification map. .................. 24 Figure 17. Fort St. Philip study area - 1978-1988 high-resolution land change analysis map. ............. 25 Figure 18. Fort St. Philip study area - 1998 high-resolution land-water classification map. .................. 26 Figure 19. Fort St. Philip study area - 1988-1998 high-resolution land change analysis map. ............ 27 Figure 20. Fort St. Philip study area - 2008 high-resolution land-water classification map. .................. 28 Figure 21. Fort St. Philip study area - 1998-2008 high-resolution land change analysis map............. 29 Figure 22. Fort St. Philip study and reference area zonal boundaries and the 1956-2008 moderate-resolution land change analysis map. .................................................................................... 32

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MRG&P Report No. 2 v

Tables

Table 1. Status of available photography, imagery, and classified land and water data within the Fort St. Philip study area. ............................................................................................................ 5 Table 2. Dominant landscape feature changes identified using visual observation of high-resolution aerial photography and digital imagery. Corresponding feature numbers are represented in Figures 5-9 for location identification. ................................................................... 18 Table 3. Summary of Fort St. Philip study area acreages, and percentages of area change, for select time periods - from high-resolution analyses. The color-ramp illustrates the type and magnitude of land change, where the darkest red represents the loss maxima and darkest green represents gain maxima. ................................................................................................... 30 Table 4. Summary of Fort St. Philip study area zonal statistics, and percentages of area change, for select time periods - from moderate-resolution analyses. The color-ramp illustrates the type and magnitude of land change, where the darkest red represents the loss maxima and the darkest green represents gain maxima. ............................................................. 33

Page 7: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MRG&P Report No. 2 vi

Summary

Quantifying the effects of active natural and constructed crevasses is critical to the planning and success of future ecosystem restoration activities. However, program stakeholders often lack the comprehensive assessments and tools necessary to quantify those short- and long-term effects. Therefore, this document has been prepared to provide a historical overview of landscape changes within the vicinity of the natural crevasses near Fort St. Philip, Louisiana.

This study utilized aerial photography, satellite imagery, and existing and newly generated land and water classifications to: (1) identify the time at which the Fort St. Philip crevasses were formed; (2) provide a pictorial account of the evolution of the Fort St. Philip crevasses and impacted wetlands; (3) evaluate land-water ratios and landscape change within the study area; (4) detect change relative to reference wetland areas; and (5) develop descriptive figures and summary statistics. These assessments, which cover decadal or greater time periods, include historical and modern landscape analyses that are based on previous methodologies developed by this study’s principal investigators.

A significant event influencing landscape change within the Fort St. Philip study area during the study period was the breaching of the eastern levee of the Mississippi River and subsequent development of the Fort St. Philip crevasse channels. Initially, the river water that was diverted through these crevasse channels physically removed significant marsh areas within the study area. These initial direct impacts were succeeded by several decades of larger regional loss patterns driven by subsidence and other episodic events (e.g, hurricanes and floods), and recent localized land gains. These increases in land area are potentially the long-term results of the Fort St. Philip crevasses, and the short-term impacts of the Coastal Wetlands Planning, Protection, and Restoration Act (CWPPRA) BS-11 delta management activities. However, for the majority of the 1956-2008 period of analysis, the crevassing of the eastern bank of the Mississippi River levee was a loss accelerant in the Fort St. Philip area.

Page 8: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MRG&P Report No. 2 vii

Preface

The research documented in this report was conducted as part of the Mississippi River Geomorphology and Potamology (MRG&P) Program. The MRG&P is part of the Mississippi River and Tributaries Program and is managed by the US Army Corps of Engineers (USACE) Mississippi Valley Division (MVD) and Districts. The MRG&P Program Manager was Freddie Pinkard and the Technical Leader was Dr. Barbara Kleiss.

The MVD Commander was BG Peter A. DeLuca. The MVD Director of Programs was Edward Belk.

Providing Mississippi River engineering direction and policy advice was the Mississippi River Commission. The Commission members were BG DeLuca, USACE; the Honorable Sam E. Angel; the Honorable R. D. James; the Honorable Norma Jean Mattei, Ph.D.; RDML Gerd F. Glang, National Oceanic and Atmospheric Administration; BG Margaret W. Burcham, USACE; and BG John S. Kem, USACE.

The US Army Engineer Research and Development Center (ERDC) conducted this research supporting the MRG&P under the purview of the Environmental Laboratory (EL), Vicksburg, Mississippi.

This report was prepared by Glenn Suir, Environmental Systems Branch (EE-C), ERDC-EL; Bill Jones, U.S. Geological Survey, National Wetlands Research Center; Adrienne Garber, Five Rivers Services, LLC, National Wetlands Research Center; and John Barras, U.S. Geological Survey, St. Petersburg Coastal and Marine Science Center–Baton Rouge Colocation Office. The report was prepared under the general supervision of Mark Graves, Chief, EE-C; Dr. Edmond J. Russo, Jr., P.E., Chief, Ecosystem Evaluation and Engineering Division, EL; Dr. Jack Davis, Deputy Director, EL; and Dr. Beth Fleming, Director, EL.

COL Jeffrey R. Eckstein was Commander of ERDC. Dr. Jeffery P. Holland was the ERDC Director.

Page 9: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MRG&P Report No. 2 viii

Unit Conversion Factors

Multiply By To Obtain

acres 4,046.873 square meters

cubic feet 0.02831685 cubic meters

feet 0.3048 meters

miles (U.S. statute) 1,609.347 meters

square miles 2.589998 E+06 square meters

Page 10: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MRG&P Report No. 2 1

1 Introduction

1.1 Background

Crevassing of the Mississippi River has significantly contributed to delta lobe formation adjacent to the river. Crevasses, which occur as large breaches or breaks in river levees, promote infilling of shallow inter-distributary ponds with sediment-laden river water, ultimately resulting in vegetated deltaic splays (Rodrigue 2003). From 1773 to 1927, the total number of Mississippi River crevasses (principally in Louisiana) reported in the literature was 1,062 (Davis 2000). During that same period, as many as 20 natural crevasse splays were active in the modern Mississippi River Delta, accounting for more than 80% of its subaerial land (Davis 2000). However, human alterations to the Mississippi River system (e.g. channel training and flood protection measures) have eliminated the majority of crevasses above river mile 42 (corresponds to the southern terminus of the east bank flood protection levee, Figure 1), thereby reducing the supply of nutrient- and sediment-rich water that is vital for the subsistence of deltaic wetlands (National Research Council 2006).

For the last half-century, Louisiana’s coastal wetlands have experienced rapid degradation (Suir et al. 2013). However, with past successes of delta progradation through natural crevassing, artificial crevasse cuts and freshwater diversions could be viable engineering techniques for utilizing nutrient- and sediment-laden water for marsh management and ecosystem restoration. With numerous artificial crevasses and freshwater diversions currently constructed or proposed, quantifying the long-term landscape changes and trends that are associated with active crevasses is critical to the planning and success of future projects.

1.2 Purpose

The primary goals of this study were to identify and quantify recent and historical land change trends from the mid-1950s through 2008 for the area surrounding the active Mississippi River levee breach near Fort St. Philip, Louisiana, and to compare the magnitude and sequencing of those changes to reference areas along the eastern bank of the Mississippi River (Breton Sound Basin).

Page 11: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MR

G&

P R

epor

t No.

2

2

Figure 1. Fort St. Philip Crevasses study location map.

Page 12: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MR

G&

P R

epor

t No.

2

3

To a

chie

ve th

ese

goal

s, th

e au

thor

s pr

opos

ed th

at g

eosp

atia

l dat

a be

ac

quir

ed, p

roce

ssed

, and

/or

gene

rate

d in

ord

er to

: (1)

iden

tify

the

even

t(s)

an

d ti

min

g at

whi

ch th

e M

issi

ssip

pi R

iver

leve

e w

as b

reac

hed,

res

ulti

ng in

th

e Fo

rt S

t. Ph

ilip

crev

asse

s; (2

) pro

vide

a p

icto

rial

acc

ount

of t

he

evol

utio

n of

the

Fort

St.

Phili

p cr

evas

ses;

(3) a

naly

ze c

hang

es in

pro

ject

ar

ea w

etla

nd la

ndsc

apes

ove

r ti

me

usin

g la

nd a

nd w

ater

cla

ssifi

cati

ons;

(4

) ana

lyze

cha

nges

to c

ompa

re th

e pr

ojec

t are

a to

ref

eren

ce a

rea

land

scap

es; a

nd (5

) dev

elop

des

crip

tive

figu

res

and

sum

mar

y st

atis

tics

.

1.3

Proj

ect a

rea

The

7,39

1-ac

re s

tudy

sit

e is

loca

ted

in s

outh

east

ern

Bre

ton

Soun

d B

asin

, w

hich

ext

ends

from

the

Mis

siss

ippi

Riv

er e

ast t

o th

e M

issi

ssip

pi R

iver

Gul

f O

utle

t, an

d so

uth

from

Bay

ou T

erre

aux

Boe

ufs

to B

apti

ste

Col

lett

e B

ayou

(F

igur

e 1)

. The

983

-mi2

bas

in, a

rem

nant

of t

he S

t. B

erna

rd D

elta

, als

o co

ntai

ns s

ever

al a

band

oned

dis

trib

utar

y ch

anne

ls in

clud

ing

Bay

ou L

a Lo

utre

, Riv

er a

ux C

hene

s, a

nd B

ayou

Lam

oque

(US

Fish

and

Wild

life

Serv

ice

(USF

WS)

200

3). I

n ad

diti

on to

thes

e ch

anne

ls, f

low

s al

so e

scap

e th

e ri

ver

thro

ugh

seve

ral n

atur

al a

nd m

an-m

ade

open

ings

in th

e ba

nk

(Fig

ure

1). T

he s

tudy

are

a is

gen

eral

ly im

pact

ed b

y ri

veri

ne o

verb

ank

flood

ing/

crev

assi

ng, t

idal

and

met

rolo

gica

l con

diti

ons,

and

rap

id s

ubsi

-de

nce.

Thi

s st

udy

will

focu

s on

the

open

ings

(cre

vass

es) a

nd th

e ar

ea o

f in

fluen

ce lo

cate

d ne

ar F

ort S

t. Ph

ilip.

Ass

essi

ng th

e sh

ort-

and

long

-ter

m la

ndsc

ape

chan

ges

that

hav

e oc

curr

ed

pre-

and

pos

t-cr

evas

sing

, and

com

pari

ng th

ose

chan

ges

to r

efer

ence

are

as,

prov

ides

val

uabl

e in

form

atio

n re

late

d to

nat

ural

cre

vass

e fo

rmat

ion

and

evol

utio

n. A

lso,

at 1

00,0

00 ft

3 /se

c (m

easu

red

duri

ng h

igh

rive

r st

age)

, the

flo

w th

roug

h th

ese

crev

asse

cha

nnel

s pr

ovid

es a

n an

alog

by

whi

ch to

as

sess

land

scap

e-le

vel i

mpa

cts

from

larg

e fr

eshw

ater

div

ersi

ons.

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MR

G&

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epor

t No.

2

4

2 M

etho

ds

Thre

e pr

imar

y ta

sks

wer

e as

soci

ated

with

this

stu

dy. T

hose

task

s w

ere:

(1

) dat

a ac

quis

ition

and

pro

cess

ing,

(2) l

ands

cape

ana

lyse

s w

ithin

the

stud

y ar

ea u

sing

hig

h-re

solu

tion

phot

ogra

phy

and

imag

ery,

and

(3) c

ompa

riso

n of

pr

ojec

t and

ref

eren

ce a

rea

land

scap

es u

sing

mod

erat

e-re

solu

tion

imag

ery.

Th

ese

asse

ssm

ents

con

sist

ed o

f his

tori

cal a

nd m

oder

n la

ndsc

ape

anal

yses

ba

sed

on m

etho

dolo

gies

and

dat

a de

velo

ped

for

prio

r co

asta

l tre

nd s

tudi

es

(Bar

ras

2009

, Bar

ras

et a

l. 20

08, L

ouis

iana

Dep

artm

ent o

f Nat

ural

R

esou

rces

(LD

NR

) 199

5, S

altu

s et

al.

2012

, Sui

r et

al.

2011

).

2.1

Dat

a ac

quis

ition

and

pro

cess

ing

Dec

adal

or

grea

ter

peri

ods

of a

naly

ses

wer

e pr

opos

ed fo

r th

is s

tudy

. H

owev

er, t

hose

per

iods

wer

e ul

timat

ely

base

d on

the

tim

e of

cre

vass

e fo

rmat

ion,

ava

ilabl

e ae

rial

pho

togr

aphy

and

cla

ssifi

ed im

ager

y, a

nd ti

me

requ

irem

ents

for

perf

orm

ing

addi

tiona

l lan

d an

d w

ater

cla

ssifi

catio

ns.

Hig

her

reso

lutio

n (<

1:65

,000

sca

le) h

isto

rica

l and

rec

ent a

eria

l pho

to-

grap

hy a

nd d

igit

al im

ager

y w

ere

acqu

ired

for

the

year

s 19

56, 1

970,

197

3,1

1974

,1 19

78, 1

989,

1 199

8, a

nd 2

008

(Tab

le 1

). T

houg

h th

e 19

98 a

nd 2

008

data

exi

st in

geo

-rec

tifie

d an

d m

osai

cked

dig

ital

form

ats,

the

1956

, 197

0,

1973

, 197

4, 1

978,

and

198

9 da

ta w

ere

only

ava

ilabl

e in

un-

rect

ified

Tag

ged

Imag

e Fi

le (T

IF) f

orm

at. T

here

fore

, all

un-r

ectif

ied

fram

es w

ere

rect

ified

us

ing

the

2008

dig

ital i

mag

ery

as th

e co

ntro

l, an

d su

bset

to th

e st

udy

area

bo

unda

ry.

The

land

cha

nge

asse

ssm

ents

(bot

h hi

gh- a

nd m

oder

ate-

reso

lutio

n)

disc

usse

d w

ithin

this

rep

ort w

ere

calc

ulat

ed u

sing

land

and

wat

er d

ata

sets

an

d m

etho

ds d

evel

oped

for

prio

r co

asta

l lan

d ar

ea c

hang

e as

sess

men

ts

(Bar

ras

2006

, 200

9; B

arra

s et

al.

1994

, 200

3, 2

008;

Cah

oon

and

Gro

at

1990

; Sal

tus

et a

l. 20

12; U

S G

eolo

gica

l Sur

vey

(USG

S) 1

980,

198

8a, 1

988b

, 20

09),

as

wel

l as

land

and

wat

er d

ata

sets

cre

ated

as

part

of t

his

stud

y (1

970

and

1998

). E

xist

ing

and

new

ly c

reat

ed la

nd a

nd w

ater

dat

a se

ts w

ere

deri

ved

from

mul

tiple

sou

rce

data

. Exi

stin

g da

ta s

ourc

es in

clud

e La

ndsa

t

1 The

se p

hoto

grap

hs w

ere

conv

erte

d to

a d

igita

l for

mat

by

the

US G

eolo

gica

l Sur

vey,

Eart

h Re

sour

ces

Obse

rvat

ion

and

Scie

nce

(ERO

S) C

ente

r usi

ng c

harg

e-co

uple

d de

vice

(CCD

) cap

ture

rath

er th

an a

fla

tbed

sca

nner

and

are

con

side

red

med

ium

-reso

lutio

n da

ta. H

owev

er, c

ompa

red

to m

oder

ate-

reso

lutio

n La

ndsa

t im

ager

y, an

d fo

r sim

plify

ing

asse

ssm

ent t

asks

, the

se p

hoto

s w

ill b

e co

nsid

ered

hi

gh-re

solu

tion

data

for t

his

stud

y.

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MR

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t No.

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5

Them

atic

Map

per

(TM

) sat

ellit

e im

ager

y ob

tain

ed fr

om th

e U

SGS

Cen

ter

for

Ear

th R

esou

rces

Obs

erva

tion

and

Sci

ence

(mod

erat

e-re

solu

tion

data

fr

om 1

988,

200

1, a

nd 2

008;

Tab

le 1

). T

hose

land

and

wat

er d

ata

sets

that

w

ere

mod

ified

from

pho

to-i

nter

pret

ed N

atio

nal W

etla

nds

Inve

ntor

y (N

WI)

ha

bita

t dat

a co

nsis

t of h

igh-

reso

lutio

n da

ta fr

om 1

956,

197

8, 1

988,

and

20

08 (T

able

1).

Add

itio

nally

, the

land

and

wat

er d

ata

sets

that

wer

e de

rive

d sp

ecifi

cally

for

this

stu

dy c

onsi

st o

f pho

to-i

nter

pret

ed, h

igh-

reso

lutio

n pa

nchr

omat

ic a

nd c

olor

infr

ared

(CIR

) aer

ial p

hoto

grap

hy fr

om 1

970

and

1998

, res

pect

ivel

y (T

able

1).

Sin

ce th

ese

data

wer

e pr

oces

sed

by v

ario

us

anal

ysts

and

cla

ssifi

ed u

sing

diff

erin

g m

etho

ds, m

easu

res

wer

e ta

ken

to

ensu

re c

ompa

tibili

ty b

etw

een

data

set

s (s

ee b

elow

).

Tabl

e 1.

Sta

tus

of a

vaila

ble

phot

ogra

phy,

imag

ery,

and

clas

sifie

d la

nd a

nd w

ater

dat

a wi

thin

the

Fort

St. P

hilip

stu

dy a

rea.

Asse

ssm

ent

Date

Da

ta T

ype

Data

Sou

rce

Scal

e Pr

oces

s/Ap

plic

atio

n

Fort St. Philip Project Area Higher Resolution (1-m resampled)

24 M

arch

19

56

Panc

hrom

atic

Ph

otog

raph

y Ar

my

Map

Ser

vice

1:

24,0

00

Aggr

egat

ed N

WI H

abita

t

8 M

arch

19

701

Panc

hrom

atic

Ph

otog

raph

y U.

S. G

eolo

gica

l Sur

vey

1:54

,800

La

nd a

nd W

ater

D

elin

eatio

n

11 A

pril

1973

Pa

nchr

omat

ic

Phot

ogra

phy3

N

ASA

- AM

ES

1:12

7,00

0 Vi

sual

Inte

rpre

tatio

n

17 O

ctob

er

1974

Pa

nchr

omat

ic

Phot

ogra

phy3

N

ASA

- JSC

1:

119,

000

Visu

al In

terp

reta

tion

15 O

ctob

er

1978

CI

R Ph

otog

raph

y4

NAS

A - A

MES

1:

65,0

00

Aggr

egat

ed N

WI H

abita

t

1 Ja

nuar

y 19

88

CIR

Phot

ogra

phy4

N

ASA

1:65

,000

Ag

greg

ated

NW

I Hab

itat

30 O

ctob

er

1989

2 CI

R Ph

otog

raph

y4

U.S.

Geo

logi

cal S

urve

y - N

APP

1:40

,000

Vi

sual

Inte

rpre

tatio

n

4 Fe

brua

ry

1998

1 D

OQQ4

La

. Oil

Spill

Coo

rdin

ator

's O

ffice

1:

40,0

00

Land

and

Wat

er

Del

inea

tion

30 O

ctob

er

2008

D

igita

l Im

ager

y4

U.S.

Geo

logi

cal S

urve

y -

Aggr

egat

ed N

WI H

abita

t

Breton Reference Area Moderate Resolution (25-m resampled)

24 M

arch

19

56

Panc

hrom

atic

Ph

otog

raph

y Ar

my

Map

Ser

vice

1:

20,0

00

Prev

ious

ly Ag

greg

ated

and

Re

sam

pled

NW

I

15 O

ctob

er

1978

CI

R Ph

otog

raph

y N

ASA

- AM

ES

1:65

,000

Pr

evio

usly

Aggr

egat

ed a

nd

Resa

mpl

ed N

WI

28 Ja

nuar

y 19

88

Land

sat 5

Im

ager

y N

ASA

- La

nd a

nd W

ater

D

elin

eatio

n

30 O

ctob

er

2001

La

ndsa

t 5

Imag

ery

NAS

A -

Land

and

Wat

er

Del

inea

tion

1 Oc

tobe

r 20

08

Land

sat 5

Im

ager

y N

ASA

- La

nd a

nd W

ater

D

elin

eatio

n 1 1

970

and

1998

land

and

wat

er d

ata

wer

e de

linea

ted

as p

art o

f thi

s st

udy.

2 198

9 ph

otog

raph

y pr

ovid

es h

ighe

r qua

lity

data

than

thos

e us

ed in

198

8 N

WI c

lass

ifica

tion.

3 Us

ed fo

r ass

essi

ng s

eque

ncin

g of

leve

e br

each

. 4 Th

e co

lor i

nfra

red

phot

ogra

phy u

sed

in th

is re

port

’s fi

gure

s ar

e di

spla

yed

in g

rays

cale

for e

ase

of c

ompa

rison

.

Page 15: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MR

G&

P R

epor

t No.

2

6

2.2

Hig

h-re

solu

tion

data

The

high

er r

esol

utio

n la

nd a

nd w

ater

dat

a th

at w

ere

used

in th

is s

tudy

wer

e de

rive

d fr

om p

hoto

grap

hy o

btai

ned

in 1

956

(1:2

4K),

197

0 (1

:58.

4K),

197

8 (1

:65K

), a

nd 1

988

(1:6

5K, m

agni

fied

to 1

:24k

for

zoom

tran

sfer

); fr

om 1

998

colo

r in

frar

ed (C

IR) p

hoto

grap

hy (1

:40K

/1 m

); a

nd fr

om 2

008

(1-m

) CIR

di

gita

l im

ager

y (T

able

1).

As

a pr

ecur

sor,

it s

houl

d be

not

ed th

at m

etho

ds

used

to d

eriv

e th

ese

land

and

wat

er d

ata

vari

ed c

onsi

dera

bly.

Lan

d an

d w

ater

dat

a fo

r th

e ye

ars

1956

, 197

8, a

nd 1

988

wer

e de

rive

d fr

om e

xist

ing

NW

I hab

itat d

ata

deve

lope

d fo

r pr

ior

coas

tal c

hara

cter

izat

ion

stud

ies

(Wic

ker

1980

, 198

1; U

SGS

1988

b; B

arra

s et

al.

1994

; Ful

ler

et a

l. 19

95).

Th

ese

habi

tat d

ata

wer

e cl

assi

fied

usin

g a

stan

dard

NW

I cla

ssifi

catio

n sc

hem

e (C

owar

din

et a

l. 19

79).

The

NW

I hab

itat

sch

eme

was

ada

pted

to

iden

tify

spec

ific

Loui

sian

a w

etla

nd h

abit

ats

usin

g co

de m

odifi

ers

(Wic

ker

1980

). T

o co

mpa

re c

hang

es in

land

and

wat

er a

rea,

the

clas

sifie

d ha

bita

t da

ta w

ere

aggr

egat

ed in

to la

nd a

nd w

ater

cat

egor

ies

usin

g a

stan

dard

cl

assi

ficat

ion

sche

me.

Lan

d fe

atur

es r

epre

sent

upl

ands

, em

erge

nt

vege

tatio

n, w

etla

nd fo

rest

, or

scru

b-sh

rub;

and

wat

er fe

atur

es r

epre

sent

any

op

en w

ater

, flo

atin

g or

sub

mer

ged

aqua

tics,

and

non

-veg

etat

ed m

ud fl

at.

For

tidal

ly-i

nflu

ence

d la

ndsc

apes

, as

with

the

Fort

St.

Phili

p st

udy

area

, de

linea

ting

land

and

wat

er fe

atur

e bo

unda

ries

from

NW

I hab

itat

dat

a is

of

ten

diff

icul

t. Fo

r th

is p

roje

ct, t

he d

elin

eatio

n w

as s

et b

etw

een

habi

tat

clas

ses

with

“R

egul

arly

Flo

oded

” an

d “I

rreg

ular

ly F

lood

ed”

wat

er r

egim

es.

Thes

e ti

dally

-inf

luen

ced

regi

mes

are

bas

ed o

n in

term

edia

te, b

rack

ish,

and

sa

line

mod

ifier

s. R

egul

arly

Flo

oded

feat

ures

rep

rese

nt a

reas

that

alte

rnat

ely

flood

and

exp

ose

the

land

sur

face

at l

east

onc

e da

ily; I

rreg

ular

ly F

lood

ed

feat

ures

are

thos

e w

here

wat

er fl

oods

the

land

sur

face

less

oft

en th

an d

aily

.

The

1970

and

199

8 la

nd a

nd w

ater

dat

a w

ere

deri

ved

from

unr

ecti

fied

panc

hrom

atic

pho

togr

aphy

and

ort

ho-r

ecti

fied

CIR

aer

ial p

hoto

grap

hy,

resp

ecti

vely

. The

197

0 ph

otos

wer

e sc

anne

d in

to a

dig

ital

form

at a

nd g

eo-

rect

ified

to a

Uni

vers

al T

rans

vers

e M

erca

tor

(UTM

) coo

rdin

ate

syst

em.

Man

ual l

and

and

wat

er c

lass

ifica

tion

s w

ere

perf

orm

ed u

sing

an

on-s

cree

n in

tera

ctiv

e "h

eads

-up"

tech

niqu

e th

at u

tiliz

es p

hoto

rad

ianc

e, c

ontr

ast,

text

ure,

and

pat

tern

rec

ogni

tion

by

whi

ch la

nd a

nd w

ater

feat

ures

wer

e de

linea

ted

dire

ctly

into

a d

igit

al G

IS (S

uir

et a

l. 20

11).

The

2008

hab

itat

dat

a w

ere

deri

ved

from

1-m

dig

ital

imag

ery

capt

ured

w

ith

the

ZI D

igit

al M

appi

ng C

amer

a. A

s pa

rt o

f ong

oing

eff

orts

by

the

USG

S to

map

Lou

isia

na’s

coa

stal

hab

itat

s, th

e 20

08 im

ager

y w

as c

lass

ified

Page 16: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MR

G&

P R

epor

t No.

2

7

usin

g th

e es

tabl

ishe

d N

WI

habi

tat c

lass

ifica

tion

sch

eme.

The

cla

ssifi

ed

habi

tat d

ata

wer

e th

en a

ggre

gate

d in

to la

nd a

nd w

ater

cat

egor

ies.

Due

to e

volv

ing

clas

sific

atio

n an

d re

ctifi

cati

on te

chni

ques

, it w

as e

ssen

tial t

o ev

alua

te in

cons

iste

ncie

s in

the

regi

stra

tion,

sca

le, a

nd m

appi

ng u

nit s

ize

of

sour

ce a

nd c

lass

ified

dat

a. T

he e

arlie

r ha

bita

t dat

a se

ts w

ere

tran

sfor

med

to

mat

ch th

e 19

98 a

nd 2

008

data

. Thi

s w

as a

chie

ved

by e

ither

re-

regi

ster

ing

the

hist

oric

line

-wor

k to

200

8 co

ntro

l poi

nts,

or

by r

aste

rizi

ng th

e hi

stor

ical

la

nd a

nd w

ater

line

-wor

k an

d ge

o-re

fere

ncin

g to

the

2008

imag

ery.

Co-

regi

ster

ing

the

data

pro

vide

s gr

eate

r co

nfid

ence

in th

e re

sults

. Add

ition

ally

, cl

assi

ficat

ion

accu

raci

es o

f tho

se la

nd a

nd w

ater

dat

a th

at w

ere

aggr

egat

ed

from

exi

stin

g N

WI d

ata

wer

e al

so a

sses

sed.

Any

mis

clas

sifie

d la

nd o

r w

ater

fe

atur

es w

ere

corr

ecte

d us

ing

the

“hea

ds-u

p” m

etho

d de

scri

bed

abov

e.

2.3

Mod

erat

e-re

solu

tion

data

The

mod

erat

e-re

solu

tion

dat

a us

ed in

this

stu

dy c

onsi

st o

f exi

stin

g La

ndsa

t 5 T

hem

atic

Map

per

(TM

) sat

ellit

e im

ager

y fr

om 1

988,

200

1, a

nd

2008

, pre

viou

sly

resa

mpl

ed to

25

m (B

arra

s 20

09; B

arra

s et

al.

2008

; Sa

ltus

et a

l. 20

12, T

able

1);

and

agg

rega

ted

1956

and

197

8 ha

bita

t dat

a (W

icke

r 19

80, 1

981)

that

wer

e ra

ster

ized

and

res

ampl

ed to

mat

ch T

M

spat

ial r

esol

utio

n (C

ahoo

n an

d G

roat

199

0). A

ll of

the

TM d

ata

that

wer

e us

ed in

this

stu

dy w

ere

clas

sifie

d us

ing

a st

anda

rd c

lass

ifica

tion

m

etho

dolo

gy to

ens

ure

repe

atab

ility

and

con

sist

ency

, as

wel

l as

to

min

imiz

e cl

assi

ficat

ion

inte

rpre

tati

on s

ubje

ctiv

ity

(Bar

ras

et a

l. 20

03).

Th

ese

met

hods

con

sist

ed o

f rad

iom

etri

c co

rrec

tion

, edg

e en

hanc

emen

t, an

d ba

nd 5

-lev

el s

licin

g of

the

TM d

ata.

Fin

al r

esam

plin

g an

d no

ise

filte

ring

wer

e pe

rfor

med

on

all d

ata

that

wer

e us

ed in

the

mod

erat

e-re

solu

tion

ass

essm

ents

(Bra

ud a

nd F

eng

1998

, Sui

r et

al.

2011

).

Page 17: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MR

G&

P R

epor

t No.

2

8

3 R

esul

ts

3.1

Aeria

l pho

togr

aphy

Exa

min

ing

hist

oric

al a

nd m

oder

n ae

rial

pho

togr

aphy

, acq

uire

d fr

om 1

956

thro

ugh

2008

, pro

vide

s a

mea

ns o

f ide

ntify

ing

and

empi

rica

lly d

ocu-

men

ting

the

land

scap

e ch

ange

s th

at h

ave

occu

rred

with

in th

e Fo

rt S

t. Ph

ilip

stud

y ar

ea. P

revi

ous

repo

rts

have

theo

rize

d th

at m

arsh

loss

in th

is a

rea

has

been

the

resu

lt of

sub

side

nce,

win

d an

d w

ave

eros

ion,

and

the

scou

ring

of

orga

nic

mar

sh s

oils

whe

n ri

ver

wat

er w

as in

trod

uced

thro

ugh

the

natu

ral

crev

asse

s ne

ar F

ort S

t. Ph

ilip

(USF

WS

2003

). T

houg

h th

e sp

ecifi

c tim

e of

br

each

ing

near

For

t St.

Phili

p ha

s ne

ver

been

doc

umen

ted,

it h

as b

een

assu

med

that

thes

e cr

evas

ses

wer

e cr

eate

d du

ring

the

maj

or M

issi

ssip

pi

Riv

er fl

ood

of 1

973

(USF

WS

2003

). F

igur

es 2

and

3 c

orre

late

bou

ndin

g ae

rial

pho

togr

aphy

and

his

tori

cal r

iver

sta

ge w

ith th

e se

quen

cing

of t

he

Mis

siss

ippi

Riv

er le

vee

brea

ch. T

he 7

Apr

il 19

73 fl

ood

stag

e pe

ak (+

7.7

ft) a

t th

e E

mpi

re g

age

(Fig

ure

2) c

orre

spon

ds to

the

pre-

, act

ive-

, and

pos

t-br

each

se

quen

ce th

at is

illu

stra

ted

in F

igur

e 3.

Figu

re 2

. Dai

ly M

issi

ssip

pi R

iver

sta

ge d

ata

(wat

er le

vel,

in fe

et) a

t Em

pire

gag

e (b

lue)

and

Ve

nice

gag

e (g

reen

), Lo

uisi

ana.

Flo

od s

tage

pea

k id

entif

ied

with

red

circ

le.

7 A

pril

1973

Page 18: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MR

G&

P R

epor

t No.

2

9

Figure 3. Aerial photography showing pre- (left pane), active- (middle pane), and post-breaching (right pane) of the Mississippi River levee near Fort St. Philip, Louisiana in 1970, 1973 (moderate-resolution photography experiencing Moiré effect), and 1974, respectively. Breach

site identified with red ovals.

Page 19: MRG&P Report No. 2 'Pictorial Account and Landscape ... · Mississippi River Geomorphology and Potamology Program MRG&P Report No. 2 January 2014 Pictorial Account and Landscape Evolution

MR

G&

P R

epor

t No.

2

10

Figu

res

4-10

pre

sent

a p

icto

rial

acc

ount

of t

he F

ort S

t. Ph

ilip

stud

y ar

ea

and

prov

ide

furt

her

evid

ence

that

the

crev

asse

s w

ere

a re

sult

of t

he 1

973

flood

(Fig

ure

6). T

hese

figu

res,

whi

ch c

onsi

st o

f pho

togr

aphy

from

195

6,

1970

, 197

8, 1

989,

199

8, a

nd 2

008

(and

the

2011

pho

tom

osai

c m

ap fr

om

the

Del

ta M

anag

emen

t at F

ort S

t. Ph

ilip

Coa

stal

Wet

land

s Pl

anni

ng,

Prot

ecti

on, a

nd R

esto

rati

on A

ct (C

WPP

RA

) pro

ject

), a

llow

for

visu

al

inte

rpre

tati

on a

nd c

ompa

riso

n of

land

scap

e fe

atur

e ex

tent

and

cha

nge.

N

otab

le la

ndsc

ape

feat

ure

chan

ges

wit

hin

the

Fort

St.

Phili

p st

udy

area

are

pr

ovid

ed in

Tab

le 2

and

iden

tifie

d in

Fig

ures

3-1

0.

3.2

Land

scap

e ar

ea a

nd c

hang

e –

Hig

h-re

solu

tion

anal

yses

Exi

stin

g an

d ne

wly

cla

ssifi

ed la

nd a

nd w

ater

dat

a pr

ovid

e vi

sual

and

co

mpu

tatio

nal a

ids

for

asse

ssin

g w

etla

nd a

rea

and

chan

ge. F

igur

es 1

1, 1

2, 1

4,

16, 1

8, a

nd 2

0 ill

ustr

ate

the

land

and

wat

er a

rea,

and

land

scap

e co

nfig

urat

ion

for t

he y

ears

195

6, 1

970,

197

8, 1

988,

199

8, a

nd 2

008.

Fig

ures

13,

15,

17,

19,

an

d 21

dep

ict l

and

and

wat

er c

hang

es fo

r seq

uent

ial p

erio

ds o

f ana

lysi

s.

Figu

re 1

1 sh

ows

a 19

56 la

ndsc

ape

that

con

sist

ed o

f 5,0

12 a

cres

of r

elat

ivel

y so

lid m

arsh

, and

2,3

79 a

cres

of w

ater

, com

pris

ed p

rim

arily

of t

he M

issi

ssip

pi

Riv

er, L

ittle

Coq

uille

Bay

, nat

ural

bay

ous,

and

min

imal

oil

and

gas

acce

ss

cana

ls. B

y 19

70 (F

igur

e 12

), th

e st

udy

area

con

sist

ed o

f 4,3

77 a

nd 3

,014

acr

es

of la

nd a

nd w

ater

, res

pect

ivel

y. T

his

amou

nts

to 6

35 a

cres

of n

et la

nd lo

ss

betw

een

1956

and

197

0 (T

able

3).

The

net c

hang

e be

twee

n 19

56 a

nd 1

970

was

ca

lcul

ated

by

subt

ract

ing

the

tota

l are

a of

land

loss

(832

acr

es) f

rom

the

tota

l ar

ea o

f lan

d ga

ins

(197

acr

es).

Thes

e m

oder

ate

land

loss

es (c

ompa

red

to

subs

eque

nt ti

me

peri

ods)

wer

e th

e pr

imar

y re

sults

of b

ay-s

ide

shor

elin

e er

osio

n (l

ikel

y ac

cele

rate

d by

Hur

rica

nes

Bet

sy a

nd C

amill

e), d

irec

t im

pact

s by

acc

ess

cana

ls, a

nd p

oten

tially

the

resu

lts o

f min

or u

nder

-cla

ssifi

catio

n of

w

ater

feat

ures

in th

e 19

56 d

ata

(Fig

ure

13; l

oss

depi

cted

in re

d). T

he g

ains

(d

epic

ted

in g

reen

) dur

ing

this

per

iod

wer

e pr

imar

ily d

ue to

the

arm

orin

g of

th

e ea

st b

ank

of th

e ri

ver.

By

1978

, the

For

t St.

Phili

p st

udy

area

con

sist

ed o

f 2,7

60 a

nd 4

,631

acr

es

of la

nd a

nd w

ater

, res

pect

ivel

y (F

igur

e 14

). T

he 1

,617

acr

es o

f net

loss

(1

,932

acr

es o

f los

s an

d 31

5 ac

res

of g

ain)

are

pos

sibl

y du

e to

the

com

bine

d ef

fect

s of

mar

sh s

cour

ing,

as

a re

sult

of t

he n

ewly

form

ed c

reva

sses

(7.7

ft

rive

r st

age

on 7

Apr

il 19

73, E

mpi

re g

age;

Tab

le 3

and

Fig

ures

2 a

nd 1

5) a

nd

subs

iden

ce (G

aglia

no 1

999)

. Sub

sequ

ent m

ajor

floo

ding

eve

nts

(i.e

. 6.3

6 ft

ri

ver

stag

e on

14

Apr

il 19

75, E

mpi

re g

age)

may

hav

e ex

acer

bate

d th

e in

itia

l sc

ouri

ng. T

he n

omin

al la

nd g

ains

dur

ing

this

per

iod

are

pres

umab

ly d

ue to

in

fillin

g an

d de

posi

tion

al p

roce

sses

as

a re

sult

of s

edim

ent-

rich

riv

er w

ater

be

ing

dive

rted

thro

ugh

the

crev

asse

cha

nnel

s.

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Figure 4. Fort St. Philip study area - 1956 high-resolution photomosaic map.

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Figure 5. Fort St. Philip study area with access canals (#1) - 1970 high-resolution photomosaic map (Table 2).

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Figure 6. Fort St. Philip study area with crevasse locations (#2), areas with major land-to-water conversion (#3), and formation of crevasse channels (#4) - 1978 high-resolution photomosaic map (Table 2).

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Figure 7. Fort St. Philip study area with areas of land-to-water conversion (#3), crevasse channel development (#4), and large impoundment area (#5) - 1989 high-resolution photomosaic map (Table 2).

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Figure 8. Fort St. Philip study area with areas of land-to-water conversion (#3), crevasse channel development (#4), and large impoundment area (#5) - 1998 high-resolution photomosaic map (Table 2).

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Figure 9. Fort St. Philip study area constructed CWPPRA BS-11 project terraces (#6) - 2008 high-resolution photomosaic map (Table 2).

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Figure 10. Delta Management at Fort St. Philip project area - 2011 high-resolution photomosaic map (USFWS 2013b).

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Table 2. Dom

inant landscape feature changes identified using visual observation of high-resolution aerial photography and digital im

agery. Corresponding feature numbers are represented in Figures 5-10 for location

identification. N

o. Features

Period Reference

1 Construction of oil and gas access canals

1956-1978 Figures 5 &

6

2 Breaching of the M

ississippi River bank 1970-1978

Figures 3, 5 & 6

3 M

ajor conversion of land to water

1978-1998 Figures 6, 7 &

8

4 Form

ation of crevasse channels 1978-2008

Figures 6, 7 & 8

5 D

evelopment of large im

poundment feature

1978-2008 Figures 7 &

8

6 Construction of CW

PPRA BS-11 project terraces1

1998-2008 Figures 9 &

10 1 CW

PPRA’s Delta M

anagement at Fort St. Philip (BS-11) Sedim

ent and Nutrient Trapping, and Outfall Managem

ent project (USFW

S 2013a).

There were 2,444 acres of land and 4,947 acres of w

ater within the study

area in 1988 (Figure 16). This amounts to a net loss of 316 acres of land

between 1978 and 1988 (Table 3). Though this net loss is significantly

reduced from the previous period of analysis, the localized land losses

(1,054) and gains (738) remained relatively high. Figure 17 show

s the form

ation of additional crevasse channels, which resulted in increased

sediment deposition on m

ud flats and substrate, and potentially in direct localized scouring and flooding (during high river flow

). Additionally,

since the study area contains broad shallow flats, localized changes are

partially due to seasonality and fluctuations in river stage, tides, and w

inds, as well as recurring aquatic vegetation.

Land loss continued through 1998, when the study area accounted for

1,780 acres of land and 5,611 acres of water (Figure 18). Though this

period experienced loss (1,080 acres) similar to the previous period, there

were significantly few

er gains from 1988 to 1998 (Figure 19). The losses

experienced during this period appear to have occurred along the fringe of m

arsh and wetland landform

s, and are consistent with subsidence, and

wind- and w

ave-induced erosion.

The 1998 to 2008 time fram

e is the only period of analysis that experienced net land gains. B

y 2008, the study area contained 2,102 acres of land, a net land gain of 322 acres (Figure 22 and Table 3). These gains are presum

ably the effects of the crevasses (gains are in close proxim

ity to crevasse chan-nels) and the results of the C

WPPR

A B

S-11 restoration project. The BS-11

project authorized the construction of terraces in the large impounded area

to the west, and artificial crevasse cuts into tw

o BS-11 Project A

reas (both of w

hich are within the Fort St. Philip study area; Figure 10). A

reas that did experience erosion during this period w

ere primarily along the fringe m

arsh near Little C

oquille Bay and are therefore assum

ed losses due to wind and

wave energy (Figure 21).

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Figure 11. Fort St. Philip study area - 1956 high-resolution land-water classification map.

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Figure 12. Fort St. Philip study area - 1970 high-resolution land-water classification map.

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Figure 13. Fort St. Philip study area - 1956-1970 high-resolution land change analysis map.

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Figure 14. Fort St. Philip study area - 1978 high-resolution land-water classification map.

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Figure 15. Fort St. Philip study area - 1970-1978 high-resolution land change analysis map.

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Figure 16. Fort St. Philip study area - 1988 high-resolution land-water classification map.

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Figure 17. Fort St. Philip study area - 1978-1988 high-resolution land change analysis map.

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Figure 18. Fort St. Philip study area - 1998 high-resolution land-water classification map.

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Figure 19. Fort St. Philip study area - 1988-1998 high-resolution land change analysis map.

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Figure 20. Fort St. Philip study area - 2008 high-resolution land-water classification map.

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Figure 21. Fort St. Philip study area - 1998-2008 high-resolution land change analysis map.

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Table 3. Summary of Fort St. Philip study area acreages, and percentages of area change, for select time periods - from high-resolution analyses. The color-ramp illustrates the type and magnitude of land

change, where the darkest red represents the loss maxima and darkest green represents gain maxima.

Period of Analysis Years

Land Area (initial)

Land Area (ending)

Area Change

Area Change1 (within period) Area Change2 f

Acres Percentage

1956 to 1970 14 5,012 4,377 -635 -13% -13%

1970 to 1978 8 4,377 2,760 -1,617 -37% -32%

1978 to 1988 10 2,760 2,444 -316 -11% -6%

1988 to 1998 10 2,444 1,780 -664 -27% -13%

1998 to 2008 10 1,780 2,102 322 18% 6%

1956 to 2008 52 5,012 2,102 -2,910 -58% -58% 1 Land change percentage is based on initial land area of the period of analysis. 2 Land change percentage is based on the 1956 land area.

The CWPPRA BS-11 restoration project provides useful ancillary informa-tion. The BS-11 project area experienced extensive loss of emergent wetlands from 1974 to 1990 (USFWS 2003). Data from the U.S. Army Corps of Engineers (Britsch and Dunbar 1993) indicate that the loss rates during that period were 4.1%/year for Project Area 1 and 1.6%/year for Project Area 2 (USFWS 2003, Figure 10). From 2002 to 2011, the amount of subaerial land within BS-11 Project Area 1 (artificial crevasse cuts and terraces) increased from 153 to 228 acres, while the land in Project Area 2 (artificial crevasse cuts) increased from 101 to 116 acres (Hymel and Breaux 2012, Figure 10). Visual comparisons between the photomosaics in Figure 9 (2008) and Figure 10 (2011) show large areas of sediment plumes and accretion in Project Areas 1 and 2. These features suggest that the sediments that are being transported through the natural Fort St. Philip crevasses (and possibly through other channelized cuts) are also being conveyed through the interior artificial crevasse cuts, and ultimately deposited within the BS-11 Project Areas.

Net land area changes for the Fort St. Philip study area are summarized in Table 3. This table contains the initial and ending acreages for each of the five sequential periods, and the overall period of analysis (1956 to 2008). The table also contains the percentage of land area change for each period, based both on that period’s initial land acreage and on the 1956 acreage. Color-ramping was assigned to the percentage of land change columns to classify the type (loss or gain) and magnitude of change. The time periods with the greatest land loss are represented with dark reds, and those with the greatest land gains are represented with dark greens. The 1956-1970 period, which contained a number of major episodic events (e.g Hurricanes

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Betsy and Camille), accounted for 13% loss of land. Of the 58% of total land loss that occurred between 1956 and 2008, 32% occurred between 1970 and 1978. This period encompassed the major Mississippi River flood of 1973. Compared to the 1970-1978 time period, the 1978-1998 period experienced significantly reduced rates of loss. The 1978-1988 loss rates were similar to those experienced prior to 1970, while the 1988-1998 rates were higher, possibly as a result of additional floods (6.4-ft river stage on 23 May 1991, 6.33-ft river stage on 17 June 1995, and 6.2-ft river stage on 5 April 1997 at the Empire gage). The final period (1998-2008) was the only period with observed net land gain; an 18% increase in 1998 land acreages, and a 6% increase in 1956 land acreages.

3.3 Landscape area and change – Moderate-resolution analyses

Landscape area change analyses, utilizing moderate-resolution imagery, were performed as a means of comparing the sequence and magnitude of land change within the Fort St. Philip study area with reference areas along the eastern bank of the Mississippi River. Reference and study area boundaries (zones) were established by adjusting (simplifying) 12-digit hydrologic unit boundaries (Figure 22). The total reference area was 658 mi2 (excluding the Fort St. Philip study area). The Fort St. Philip study area boundary coincides with zone 10, while the other zones constitute the reference areas. Zonal statistics were calculated for each zone using moderate resolution (25-m) land and water imagery that was generated using resampled 1956 and 1978 NWI data, and classified 1988, 2001, and 2008 Landsat 5 TM imagery (Barras et al. 2008). Figure 22 is an example of the land change analysis that was performed for all sequential periods within, and including, the 1956 to 2008 end points. The land change image in Figure 22 shows significant land loss in the northwestern zones (1-6; predominantly hurricane impacts; Barras et al. 2010; Barras 2006, 2009) and southeastern zones (subsidence and wind/wave impacts in zones 10-16; and significant hurricane impacts in 13-16; Barras 2006, 2007), and sparse land loss within the central zones (7-9; with minor regional scale impacts from Hurricane Katrina in zone 7). Gains that have resulted from ecosystem restoration activities are also identifiable in Figure 22, specifi-cally the CWPPRA MR-09 Delta Wide Crevasses project, which is in the bounds of zones 12, 13, 14, and 15.

Land area summaries by zone and date are included in Table 4. This table also includes percentages of land change by periods of analysis, which like Table 3, are color-ramped to illustrate the type and magnitude of land change. The time periods and zones with the greatest land loss are

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Figure 22. Fort St. Philip study and reference area zonal boundaries and the 1956-2008 moderate-resolution land change analysis map.

represented with dark reds, and those with the greatest land gains are represented with dark greens. In 1956, zone 10 accounted for 5,228 acres of land (calculated using moderate-resolution data). By 2008, only 2,520 acres remained – a loss of 2,708 acres (51.8%, Table 4). The majority of that loss (46.7%) occurred during the period when the crevassing occurred near Fort St. Philip. Compared to zone 10, most of the reference zones experienced more gradual landscape changes over time, with the exceptions of zones 12, 13, and 14. However, those zones received significant restoration benefits from the MR-09 project (see land gains between 1998 and 2001). A more detailed investigation with finer temporal resolution, linked to known episodic events, would provide more confidence in landscape analyses using moderate-resolution data.

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Table 4. Summary of Fort St. Philip study area zonal statistics, and percentages of area change, for select time periods - from moderate-resolution analyses. The color-ramp illustrates the type and magnitude of land change, where the

darkest red represents the loss maxima and the darkest green represents gain maxima.

Zone

Land Area (acres) Land Change (percentage)

1956 1978 1988 2001 2008 1956-1978 1978-19881 1988-20011 2001-20081 1956-2008

1 26,201 23,602 24,082 23,333 17,833 -9.9% 1.8% -2.9% -21.0% -31.9%

2 16,787 13,418 13,404 13,900 14,418 -20.1% -0.1% 3.0% 3.1% -14.1%

3 33,339 28,894 28,506 28,075 15,541 -13.3% -1.2% -1.3% -37.6% -53.4%

4 12,779 9,845 10,613 9,916 8,285 -23.0% 6.0% -5.5% -12.8% -35.2%

5 23,573 20,857 20,457 19,343 13,962 -11.5% -1.7% -4.7% -22.8% -40.8%

6 27,336 23,812 23,827 23,328 19,220 -12.9% 0.1% -1.8% -15.0% -29.7%

7 17,207 15,900 16,246 16,104 16,035 -7.6% 2.0% -0.8% -0.4% -6.8%

8 14,181 13,487 13,379 13,267 13,427 -4.9% -0.8% -0.8% 1.1% -5.3%

9 10,907 9,952 9,887 9,468 9,581 -8.8% -0.6% -3.8% 1.0% -12.2%

10 5,228 2,787 2,467 2,505 2,520 -46.7% -6.1% 0.7% 0.3% -51.8%

11 8,718 6,848 5,559 4,311 4,144 -21.5% -14.8% -14.3% -1.9% -52.5%

12 23,476 13,166 9,783 12,123 13,001 -43.9% -14.4% 10.0% 3.7% -44.6%

13 14,510 9,863 9,941 11,967 10,294 -32.0% 0.5% 14.0% -11.5% -29.1%

14 19,216 11,287 10,948 11,815 8,920 -41.3% -1.8% 4.5% -15.1% -53.6%

15 13,147 8,827 7,700 7,370 4,862 -32.9% -8.6% -2.5% -19.1% -63.0%

16 24,752 15,894 15,167 18,025 12,591 -35.8% -2.9% 11.5% -22.0% -49.1%

1 Land change percentage is based on 1956 land area.

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4 Conclusions

This study identified and quantified land changes within the Fort St. Philip study area, and compared those changes to reference areas along the eastern bank of the lower Mississippi River. The assessments performed as part of this study were based on aerial photography and satellite imagery, as well as representative land and water data for the years 1956, 1970, 1978, 1988/89, 1998, 2001, and 2008. It should be noted that inconsistencies in area and percentage of change between the higher and moderate-resolution analyses are largely due to the reduction in precision with increasing grain (pixel) size.

A significant event influencing landscape change within the Fort St. Philip study area during the study period was the breaching of the eastern levee of the Mississippi River and subsequent development of the Fort St. Philip crevasse channels. Initially, the river water that was diverted through these crevasse channels physically removed significant marsh areas within the study area. These initial direct impacts were succeeded by several decades of larger regional loss patterns driven by subsidence (Gagliano 1999) and other episodic events (e.g, hurricanes and floods; Barras 2009), and recent localized land gains. These increases in land area are poten-tially the long-term results of the Fort St. Philip crevasses, and the short-term impacts of the CWPPRA BS-11 delta management activities. How-ever, for the majority of the 1956-2008 period of analysis, the crevassing of the eastern bank of the Mississippi River levee was a loss accelerant in the Fort St. Philip area.

The decadal comparison periods used in this study provide useful long-term trends, but they can potentially obscure short-term land and water variation. Additionally, variations in tidal and river regimes at the time of geospatial data acquisition may exacerbate or minimize actual loss trends. These can be considerable limitations, since Breton Sound contains multiple complex environmental conditions that may confound trend trajectories. Embedded within the decadal comparison periods are landscape changes that are typically caused by episodic events (e.g. hurricanes or major floods) that are super-imposed over subsidence-induced loss or losses caused by other processes (e.g. sea level rise, frontal passages, tidal variations, sediment deficiencies, etc.).

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References Barras, J., S. Beville, D. Britsch, S. Hartley, S. Hawes, J. Johnston, P. Kemp, Q. Kinler, A.

Martucci, J. Porthouse, D. Reed, K. Roy, S. Sapkota, and J. Suhayda. 2003. Historical and projected coastal Louisiana land changes 1978–2050, Appendix B of Louisiana Coastal Area (LCA), Louisiana Ecosystem Restoration Study. U.S. Geological Survey Open-File Report 2003-334, available online at http://pubs.er.usgs.gov/usgspubs/ofr/ofr03334

Barras, J. A. 2006. Land area change in coastal Louisiana after the 2005 hurricanes—a series of three maps. U.S. Geological Survey Open-File Report 2006-1274, available online at http://pubs.usgs.gov/of/2006/1274/

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REPORT DOCUMENTATION PAGE Form Approved

OMB No. 0704-0188 Public reporting burden for this collection of information is estimated to average 1 hour per response, including the time for reviewing instructions, searching existing data sources, gathering and maintaining the data needed, and completing and reviewing this collection of information. Send comments regarding this burden estimate or any other aspect of this collection of information, including suggestions for reducing this burden to Department of Defense, Washington Headquarters Services, Directorate for Information Operations and Reports (0704-0188), 1215 Jefferson Davis Highway, Suite 1204, Arlington, VA 22202-4302. Respondents should be aware that notwithstanding any other provision of law, no person shall be subject to any penalty for failing to comply with a collection of information if it does not display a currently valid OMB control number. PLEASE DO NOT RETURN YOUR FORM TO THE ABOVE ADDRESS. 1. REPORT DATE (DD-MM-YYYY)

January 2014 2. REPORT TYPE

Final report 3. DATES COVERED (From - To)

4. TITLE AND SUBTITLE

Pictorial Account and Landscape Evolution of the Crevasses Near Fort St. Philip, Louisiana

5a. CONTRACT NUMBER

5b. GRANT NUMBER

5c. PROGRAM ELEMENT NUMBER

6. AUTHOR(S)

Glenn M. Suir, William R. Jones, Adrienne L. Garber, and John A. Barras

5d. PROJECT NUMBER

5e. TASK NUMBER

5f. WORK UNIT NUMBER

7. PERFORMING ORGANIZATION NAME(S) AND ADDRESS(ES) 8. PERFORMING ORGANIZATION REPORT NUMBER

U.S. Army Engineer Research and Development Center, Environmental Laboratory 3909 Halls Ferry Road, Vicksburg, MS 39180-6199;

US Geological Survey National Wetlands Research Center 700 Cajundome Boulevard, Lafayette, LA 70506;

Five Rivers Services, LLC National Wetlands Research Center 700 Cajundome Boulevard, Lafayette, LA 70506;

US Geological Survey, Coastal and Marine Science Center 600 Fourth Street South, St. Petersburg, FL 33701

MRG&P Report No. 2

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14. ABSTRACT Quantifying the effects of active natural and constructed crevasses is critical to the planning and success of future ecosystem restoration activities. This document provides a historical overview of landscape changes within the vicinity of the natural crevasses near Fort St. Philip, Louisiana. A significant event influencing landscape change within the Fort St. Philip study area was the breaching of the eastern levee of the Mississippi River. Initially, the river water that was diverted through these crevasse channels physically removed significant marsh areas within the study area. These initial direct impacts were succeeded by several decades of larger regional loss patterns driven by subsidence and other episodic events (e.g, hurricanes and floods), and recent localized land gains. These increases in land area are potentially the long-term results of the Fort St. Philip crevasses, and the short-term impacts of delta management activities. However, for the majority of the 1956-2008 period of analysis, the crevassing of the eastern bank of the Mississippi River levee was a loss accelerant in the Fort St. Philip area.

15. SUBJECT TERMS Crevasses Ecosystem restoration

Fort St. Philip, Louisiana Landscape change Wetlands

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