fe 537 fall 2007 fe 537: hillslope and watershed fe 537 oregon state university benchmark papers...
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FE 537
Oregon State University
FE 537FE 537: : HillslopeHillslope and and Watershed HydrologyWatershed Hydrology
Taught by:
Jeff McDonnell Dept. of Forest Engineering
Oregon State University
Fall 2007
Course delivered to:
Course development funded by:
FE 537
Oregon State University
This lectureThis lecture
What are the main questions that this What are the main questions that this course will address?course will address? IntroductionsIntroductions Grading, readings, project and other class Grading, readings, project and other class
businessbusiness This course in the context of water This course in the context of water resource issues locally, nationally and resource issues locally, nationally and internationallyinternationally
FE 537
Oregon State University
This course addresses 3 basic questionsThis course addresses 3 basic questions
Where does water Where does water go when it rains?go when it rains? How long does it How long does it
reside in the reside in the catchmentcatchment?? What What flowpathflowpath
does the water take does the water take to the stream?to the stream?
Kevin McGuire
FE 537
Oregon State University
“It may seem as though a great deal is known about how, and from where, water gets from rainfall through hillslopes into streams, at least for some areas. There are, however, still major difficulties when we try either to particularize or generalize from our present knowledge”
Andy Pearce, 1990 (Water Resources Research, p. 3046)
FE 537
Oregon State University
Why such a class?Why such a class?
http://hydrology.pnl.gov/forest.asp
FE 537
Oregon State University
Why the need Why the need for this process for this process understanding?understanding?
FE 537
Oregon State University
Traditional watershed hydrologyTraditional watershed hydrology
Gordon Grant
FE 537
Oregon State University
http://www.mdbc.gov.au/education/basinkids/kidsencyclopaedia/salinity.htm
New problems that watershed hydrologists are tackling
FE 537
Oregon State University Uhlenbrook, McDonnell and Leibundgut, 2001
We will open the black box of hillslope and catchment processes…
…we’ll search for macroscale laws…..
FE 537
Oregon State University
HillslopesHillslopes are a fundamental landscape are a fundamental landscape unitunit
Photo by Jim Kirchner, UC Berkeley
FE 537
Oregon State University
WeWe’’ll explore how ll explore how hillslopeshillslopes filter filter rainfall inputs to watershedsrainfall inputs to watersheds
Time (Julian Days)
Fl ow
(L /s
)
FE 537
Oregon State University
WeWe’’ll counter this ideall counter this idea
Jan Hopmans, UC Davis
FE 537
Oregon State University From Kirkby, 1979
With this oneWith this one
FE 537
Oregon State University K
urt R oth, U
niversity H eidelberg, G
erm any
0.01 m 1 m
M arkus W
eiler, U B
C
100 m
10,000 m
Jim Kirchner, UC Berkeley
Markus Weiler, UBCWeiler and McDonnell, WRR in review
…….and we.and we’’ll find a multill find a multi--scale, complex system scale, complex system with nonwith non--linear network behavior at all scaleslinear network behavior at all scales
FE 537
Oregon State University
The The hillslopehillslope hydrology grand hydrology grand challengechallenge
Sivapalan, 2006 Encyclopedia of Hydrological Sci.
FE 537
Oregon State University
What we need to know (but do not with today’s process understanding)
Takahiro Sayama, used with permission
FE 537
Oregon State University
Course detailsCourse details
FE 537
Oregon State University
IntroductionsIntroductions
Me (see web page)Me (see web page) http://http://www.cof.orst.edu/cof/fe/watershdwww.cof.orst.edu/cof/fe/watershd
You (self introductions)You (self introductions) Who you areWho you are Your backgroundYour background What you are now studyingWhat you are now studying
FE 537
Oregon State University
AcknowledgementsAcknowledgements some of the some of the recent OSU PhDs and Post Docs whose ideas have recent OSU PhDs and Post Docs whose ideas have
contributed to this coursecontributed to this course
Fabrizio Fabrizio FeneciaFenecia, TU Delft, TU Delft Nick Hjerdt, now Swedish Agricultural UniversityNick Hjerdt, now Swedish Agricultural University April James, NC State UniversityApril James, NC State University Mario Martina, now University of Bologna Mario Martina, now University of Bologna Brian McGlynn, now Montana State UniversityBrian McGlynn, now Montana State University Kevin McGuire, now Plymouth State UniversityKevin McGuire, now Plymouth State University Jan Seibert, now Stockholm UniversityJan Seibert, now Stockholm University Ilja Tromp van Meerveld, now Simon Fraser UniversityIlja Tromp van Meerveld, now Simon Fraser University Taro Uchida, now Japan Ministry of WorksTaro Uchida, now Japan Ministry of Works Kellie Vache, now Giessen UniversityKellie Vache, now Giessen University Willem Willem vanVerseveldvanVerseveld, now Lippmann Institute, now Lippmann Institute Markus Weiler, now University of British ColumbiaMarkus Weiler, now University of British Columbia
FE 537
Oregon State University
Labs this termLabs this term
Chris Graham, PhD StudentChris Graham, PhD Student Plot Scale (Oct 11)Plot Scale (Oct 11)
Luisa Hopp, Post DocLuisa Hopp, Post Doc HillslopeHillslope Scale (Nov 1)Scale (Nov 1)
Takahiro Sayama, Post DocTakahiro Sayama, Post Doc CatchmentCatchment Scale (Nov 15)Scale (Nov 15)
FE 537
Oregon State University
FE 537
Oregon State University
Virtual lectures….if you ever suffer from insomnia
FE 537
Oregon State University
Course StructureCourse Structure
PowerpointPowerpoint lectureslectures Interactive question and answer as much Interactive question and answer as much
as possibleas possible Please interruptPlease interrupt and ask questions and ask questions
whenever something is unclear or you whenever something is unclear or you would like to add a commentwould like to add a comment——this will add this will add greatly to the learning experience for greatly to the learning experience for everyone!everyone!
FE 537
Oregon State University
Good basic materialGood basic material
FE 537
Oregon State University
Advanced materialAdvanced material
FE 537
Oregon State University
Journals you should consultJournals you should consult
FE 537
Oregon State University
A good book A good book to consult if to consult if you are new you are new
to the areato the area
FE 537
Oregon State University
The Tarboton web moduleThe Tarboton web module for those without a hydro backgroundfor those without a hydro background
FE 537
Oregon State University
FE 537
Oregon State University
The new Encyclopedia of Hydrological The new Encyclopedia of Hydrological SciencesSciences
FE 537
Oregon State University
Course TextCourse Text
FE 537
Oregon State University
Benchmark PapersBenchmark Papers
Horton, RE, 1933, The role of infiltration in the hydrological cHorton, RE, 1933, The role of infiltration in the hydrological cycleycle, , Trans. Amer. Trans. Amer. GeophysGeophys. Un.,. Un., 14, 44614, 446--460.**460.** Horton, RE, 1936, Maximum groundwater levels, Horton, RE, 1936, Maximum groundwater levels, Trans. Amer. Trans. Amer. GeophysGeophys. Un.,. Un., 17(2), 34417(2), 344--357.357. Hoover, MD and Hoover, MD and HurshHursh, CR, 1943, Influence of topography and soil, CR, 1943, Influence of topography and soil-- depth on runoff from forest land, depth on runoff from forest land, Trans. Amer. Trans. Amer. GeophysGeophys. Un.. Un., 24, , 24, 693693--697697 CappusCappus, P, 1960, Bassin versant exp, P, 1960, Bassin versant expéérimental drimental d’’AlranceAlrance: : éétudes des tudes des lois de llois de l’é’écoulement. Application au calcul et coulement. Application au calcul et àà la prla préévision des dvision des déébits. bits. La Houille BlancheLa Houille Blanche A. 493A. 493--520.520. Tsukamoto, Y., 1961, An experiment on subsurface flow, Tsukamoto, Y., 1961, An experiment on subsurface flow, J. Japanese J. Japanese Soc. ForestrySoc. Forestry, 45, 186, 45, 186--190.190. Hewlett, JD and Hewlett, JD and HibbertHibbert, AR, 1963, Moisture and energy conditions , AR, 1963, Moisture and energy conditions within a sloping soil mass during drainage, within a sloping soil mass during drainage, J. J. GeophysGeophys. Res.. Res., 68, , 68, 10811081--108
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