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-
1167
Journal of Coastal Research, Vol. 22, No. 5, 2006
Fig
ure
3fr
om‘‘D
une
Lan
dsca
peR
ejuv
enat
ion
byIn
tend
edD
esta
biliz
atio
nin
the
Am
ster
dam
Wat
erSu
pply
Dun
es’’
byS.
M.A
rens
and
L.H
.W.T
.Gee
len,
pp.1
094–
1107
.C
oppi
cedu
nes
form
edby
buri
alof
shru
bs(A
pril
2000
).
-
1168
Journal of Coastal Research, Vol. 22, No. 5, 2006
Fig
ure
4fr
om‘‘D
une
Lan
dsca
peR
ejuv
enat
ion
byIn
tend
edD
esta
biliz
atio
nin
the
Am
ster
dam
Wat
erSu
pply
Dun
es’’
byS.
M.A
rens
and
L.H
.W.T
.Gee
len,
pp.1
094–
1107
.P
hoto
grap
hof
the
cent
ralp
art
ofth
ear
ea,f
acin
gno
rth
(Apr
il20
00).
-
1169
Journal of Coastal Research, Vol. 22, No. 5, 2006
Fig
ure
7fr
om‘‘D
une
Lan
dsca
peR
ejuv
enat
ion
byIn
tend
edD
esta
biliz
atio
nin
the
Am
ster
dam
Wat
erSu
pply
Dun
es’’
byS.
M.
Are
nsan
dL
.H.W
.T.
Gee
len,
pp.
1094
–110
7.S
hado
wdu
nes
form
edaf
ter
the
esta
blis
hmen
tof
salt
wor
t(S
also
laka
li;J
uly
1999
).
-
1170
Journal of Coastal Research, Vol. 22, No. 5, 2006
Figure 11 from ‘‘Dune Landscape Rejuvenation by Intended Destabilization in the Amsterdam Water Supply Dunes’’ by S.M. Arens and L.H.W.T. Geelen, pp.1094–1107. Year-to-year variation in sand burial; from top to bottom: summer 1999; winter and summer 2000; and winters 2001, 2002, and 2003.
-
1171
Journal of Coastal Research, Vol. 22, No. 5, 2006
Figure 11 from ‘‘Dune Landscape Rejuvenation by Intended Destabilization in the Amsterdam Water Supply Dunes’’ by S.M. Arens and L.H.W.T. Geelen, pp.1094–1107. Continued.
-
1172
Journal of Coastal Research, Vol. 22, No. 5, 2006
Figure 4 from ‘‘Use of Airborne Hyperspectral Data and Laserscan Data to Study Beach Morphodynamics along the Belgian Coast’’ by Bart Deronde, RikHouthuys, Walter Debruyn, Dirk Fransaer, Vera Van Lancker, and Jean-Pierre Henriet, pp. 1108–1117. Classification image (2000 survey) of the beachbetween Blankenberge and Zeebrugge from the Spectral Angle Mapper classifications. Eight different sand types could be distinguished (labeled 2–9 inthe legend; class 1 is water and class 10 is vegetation).
Figure 7 from ‘‘Use of Airborne Hyperspectral Data and Laserscan Data to Study Beach Morphodynamics along the Belgian Coast’’ by Bart Deronde, RikHouthuys, Walter Debruyn, Dirk Fransaer, Vera Van Lancker, and Jean-Pierre Henriet, pp. 1108–1117. Classification image (2001 survey) of the beach nearKnokke-Zoute from the Spectral Angle Mapper classifications. Eight different sand types can be distinguished (labeled 2–9 in the legend; class 1 is waterand class 10 is vegetation). The numbers ranging from 235 to 247 are beach survey sections.
-
1173
Journal of Coastal Research, Vol. 22, No. 5, 2006
Fig
ure
3fr
om‘‘A
sses
smen
tof
Dam
ages
from
Rec
reat
iona
lA
ctiv
itie
son
Coa
stal
Dun
esof
the
Sout
hern
Bal
tic
Sea’
’by
Ral
fG
rune
wal
d,pp
.11
45–1
157.
Stu
dysi
te11
:dun
esw
ithi
nth
eho
lida
yre
sort
ofK
arls
hage
nsh
owin
gcl
ear
sign
sof
heav
ydi
stur
banc
efr
omtr
ampl
ing.
-
1174
Journal of Coastal Research, Vol. 22, No. 5, 2006
Fig
ure
4fr
om‘‘A
sses
smen
tof
Dam
ages
from
Rec
reat
iona
lA
ctiv
itie
son
Coa
stal
Dun
esof
the
Sout
hern
Bal
tic
Sea’
’by
Ral
fG
rune
wal
d,pp
.11
45–1
157.
Stu
dysi
te1:
dune
son
Wol
inIs
land
show
ing
nom
ajor
sign
sof
hum
andi
stur
banc
e.
-
1175
Journal of Coastal Research, Vol. 22, No. 5, 2006
Fig
ure
7fr
om‘‘A
sses
smen
tof
Dam
ages
from
Rec
reat
iona
lA
ctiv
itie
son
Coa
stal
Dun
esof
the
Sout
hern
Bal
tic
Sea’
’by
Ral
fG
rune
wal
d,pp
.11
45–1
157.
Bip
lot
wit
hm
ulti
dim
ensi
onal
scal
ing
(MD
S)
and
Bra
y-C
urti
sD
issi
mil
arit
yba
sed
onsp
ecie
sab
unda
nce
data
wit
hth
eus
eof
(A)
only
data
from
site
1(W
olin
,un
dist
urbe
d),
whi
chgr
oups
onth
eup
per
righ
t,an
dsi
te11
(Kar
lsha
gen,
heav
ily
dist
urbe
d),w
hich
grou
psin
the
low
erle
ftan
d(B
)da
tafr
omal
l12
stud
ysi
tes
(264
plot
san
d14
5di
ffer
ent
spec
ies)
.
-
Journal of Coastal Research, Vol. 22, No. 5, 2006
CO
AS
TA
LP
HO
TO
GR
AP
HB
YH
AN
SH
AN
SO
N
Gu
anab
ara
Bay
and
Pão
de
Açú
car
(Su
gar
Loa
f),
Rio
de
Jan
eiro
,R
J,
Bra
zil.
Th
ese
coas
tal
feat
ure
sar
ere
lict
sof
the
hu
mid
trop
ical
wea
ther
ing
cycl
ew
her
ela
rge
core
ston
esar
ele
ftbe
hin
das
resi
dual
saf
ter
the
fria
ble
rego
lith
isst
ripp
edaw
ayby
surfi
cial
proc
esse
s.C
han
ges
inba
sele
vel
(mea
nse
ale
vel)
and
swin
gsin
the
clim
atic
regi
me
(wet
and
dry
cycl
es)
prod
uce
inte
nse
chem
ical
wea
ther
ing
man
tles
duri
ng
lon
gst
able
phas
es.T
he
pedo
gen
icm
antl
esar
eer
oded
duri
ng
un
stab
ledr
ycl
imat
icph
ases
.Pos
tgla
cial
sea-
leve
lris
efl
oode
dth
eco
asta
lval
leys
and
isol
ated
the
inse
lber
gsat
sea.
(Coa
stal
Ph
otog
raph
byH
ans
Han
son
,D
epar
tmen
tof
Wat
erR
esou
rces
En
gin
eeri
ng,
Lu
nd
Un
iver
sity
,Sw
eden
.)
-
Journal of Coastal Research, Vol. 22, No. 5, 2006
CO
AS
TA
LP
HO
TO
GR
AP
HB
YH
AN
SH
AN
SO
N
Bea
chse
ttin
gin
Baı́
ad
eP
arat
i,R
J,B
razi
lsh
owin
ga
typ
ical
fish
erm
an’s
hou
se.W
hil
eso
me
coas
tal
segm
ents
ofth
est
ates
ofS
aoP
aulo
and
Rio
deJa
nei
roar
eh
eavi
lyu
rban
ized
,afe
wst
retc
hes
ofco
ast
are
un
spoi
led
and
can
only
bere
ach
edby
shal
low
draf
tbo
ats.
Wh
ite
san
dbe
ach
esco
mpo
sed
ofsi
lici
clas
itic
sedi
men
ts(q
uar
tzan
dfe
ldsp
ar)
mak
eu
pm
ost
beac
hes
alon
gth
isco
ast.
Alt
hou
ghth
isis
ah
igh
-en
ergy
coas
t,so
me
curv
edh
eadl
and-
bay
beac
hes
are
part
iall
ysh
elte
red
from
inci
den
tw
aves
.(C
oast
alP
hot
ogra
phby
Han
sH
anso
n,
Dep
artm
ent
ofW
ater
Res
ourc
esE
ngi
nee
rin
g,L
un
dU
niv
ersi
ty,S
wed
en.)
-
Journal of Coastal Research, Vol. 22, No. 5, 2006
CO
AS
TA
LP
HO
TO
GR
AP
HB
YH
AN
SH
AN
SO
N
Th
eco
ast
and
vill
age
ofB
arra
do
Un
a,S
P,
Bra
zil.
Asp
itis
form
edat
the
mou
thof
the
Un
aR
iver
.T
his
hea
dlan
dba
y-be
ach
sett
ing
isch
arac
teri
zed
byla
rge
sedi
men
tfl
uxe
sfr
omth
eh
inte
rlan
dth
atfe
edsp
itde
velo
pmen
tan
dn
atu
rall
yre
nou
rish
the
bay
beac
h.
Th
esp
it(p
hot
ofo
regr
oun
d)ly
ing
dow
ndr
ift
ofth
ein
let,
isst
abil
ized
byve
geta
tion
init
sce
ntr
alpo
rtio
nbu
tov
erw
ash
edfa
rth
erdo
wn
drif
t(t
oth
eri
ght)
.S
imil
arh
eadl
and
bay
beac
h-i
nle
tge
omor
phic
sett
ings
exis
tth
rou
ghou
tth
eB
razi
lian
sou
ther
nco
ast.
Usu
ally
the
mig
rati
onpa
thw
ayof
the
tida
lin
lets
isin
terr
upt
edby
the
hea
dlan
dan
dth
ein
let
loca
tion
isst
abil
ized
adja
cen
tto
it.
(Coa
stal
Ph
otog
raph
byH
ans
Han
son
,D
epar
tmen
tof
Wat
erR
esou
rces
En
gin
eeri
ng,
Lu
nd
Un
iver
sity
,Sw
eden
.)
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