Vegetation & Landscape Questions: Predict interactions hydrology, vegetation, land use, hydraulics (gH20 & surface) of floodplains. – Ex: Rio Puerco, NM:

Slides:



Advertisements
Similar presentations
Trends in Suspended Sediment Input to the San Francisco Bay from Local Tributaries Presented by Setenay Bozkurt Philip Williams &
Advertisements

How will SWOT observations inform hydrology models?
2. Research Aim and Objectives To assess the hypothesis that rural land management can be used to minimise flood and drought risk simultaneously 1) To.
EROS (Crave & Davy, 2001) “Stochastic model of erosion– sedimentation processes, based on cellular automata, which mimics the natural variability of climatic.
The Climate and the Human Activities The Climate and the Human Activities Natural Variations of the Water Cycle Natural Variations of the Water Cycle Water.
Improving soils data for better vegetation modeling Wendy Peterman, Dominique Bachelet Conservation Biology Institute  Abstract Over.
Massive Porites sp. corals as indicators of historical changes in river runoff: A case study for Antongil Bay (Masoala National Park, NE Madagascar ) J.
Rivers are formed by erosion due to Running Water.
Nidal Salim, Walter Wildi Institute F.-A. Forel, University of Geneva, Switzerland Impact of global climate change on water resources in the Israeli, Jordanian.
Cumulative Impact Estimation For Landscape Scale Forest Planning Finn Krogstad & Peter Schiess Forest Engineering, U. Washington.
Hydrology River Ecosystems and Humans. Dimensions of river ecosystems Longitudinal Lateral Vertical Temporal 2.
Forest Hydrology Issue: Interaction of forests, fish, and climate One of the dominant pathways by which land cover change affects freshwater fish habitat.
S. Fork Nooksack River, WA. Reasons for Land Clearing Agriculture Lumber Mining Urban Development.
Landslide Disturbance 1 – Landslides, also called debris flows, can rapidly change the landscape of riparian zones. 2 – The sudden movement of debris and.
Abstract Upland areas of the Willamette Basin are associated with a long history of logging and related road construction. Sediment derived from forested.
Landuse change impact on the carbon balance at highly modified floodplains a systematic approach for combined emission reduction and landuse optimalization.
ic.ucsc.edu Sytsma 2005 Attiwill et al
Mountains: Erosion. Erosion Sediment Regime Sediment “regime” of a river is set by the amount and size of material delivered from both hillslopes and.
Lecture ERS 482/682 (Fall 2002) Why watersheds? ERS 482/682 Small Watershed Hydrology.
Fundamentals of River Restoration and Salmonid Fisheries OWEB, 1999, Fundamentals of River Restoration and Salmonid Fisheries OWEB, 1999, Fundamentals.
Overview of Watershed Systems
It’s Our Nature to Know Alberta Biodiversity Monitoring Institute A Geographically- Broad Assessment of Rangeland Ecosystem Services Shannon White,
Tim Beechie NOAA Fisheries, Seattle Incorporating climate change into restoration planning.
Characterizing Future Climate – Information Needs.
Suggested Guidelines for Geomorphic aspects of Anadromous Salmonid Habitat Restoration proposals G. Mathias Kondolf.
Page 1 Met Office contribution to RL5 Task ‘Large-scale interactions between atmospheric moisture and water availability - coupling of atmospheric.
Standards for Ecologically Successful River Restoration Palmer et al., 2005, Standards for Ecologically Successful River Restoration Palmer et al., 2005,
Temporal and spatial patterns of basin scale sediment dynamics and yield.
Nicole Gasparini Arizona State University Landscape Modeling.
GGR 206 Instructor: Office: Telephone: Teaching Assistant Office: Telephone: Introduction to Hydrology J. M. Chen Room 305, 45 St. George.
Oregon Case Studies Ryan Johnson. Studies  The response of impounded sediment to a culvert replacement project on Sutter Creek, a tributary of Honey.
Dr Richard Johnson, Mountain Environments, UK.  Lead Partner: Germany: Research Institute of Forest Ecology and Forestry  Partner countries: Germany,
How do humans affect watersheds and the hydrologic cycle ?
PNAMP Habitat Status and Trends Monitoring Management Question: Are the Primary Habitat Factors Limiting the Status of the Salmon and Steelhead Populations.
Seifu A Tilahun School of Civil & Water Resources Engineering,BDU Storm Runoff and soil erosion processes on the Ethiopian highland.
Soil Erosion TSM 352 Land and Water Management Systems.
Inland Wetlands Alternate Names: Marshes, bogs, swamps Presented by: VC and AMB.
Numerical models of landscape evolution Mikaël ATTAL Marsyandi valley, Himalayas, Nepal Acknowledgements: Jérôme Lavé, Peter van der Beek and other scientists.
The hydrological cycle of the western United States is expected to be significantly affected by climate change (IPCC-AR4 report). Rising temperature and.
Watersheds Chapter 9. Watershed All land enclosed by a continuous hydrologic drainage divide and lying upslope from a specified point on a stream All.
The NOAA Hydrology Program and its requirements for GOES-R Pedro J. Restrepo Senior Scientist Office of Hydrologic Development NOAA’s National Weather.
Prof. K.T. Joseph. The key components of a flood management and prevention system will incorporate Digital terrain model of the.
CHANGING EARTH’S SURFACE Water Erosion. Udden-Wentworth Scale.
Chapter 7, Lesson 2 Landforms runoff tributary watershed sediment meander flood plain delta water gap canyon valley dune landslide.
How do humans affect watersheds and the hydrologic cycle ?
How much water will be available in the upper Colorado River Basin under projected climatic changes? Abstract The upper Colorado River Basin (UCRB), is.
Impacts of Landuse Management and Climate Change on Landslides Susceptibility over the Olympic Peninsula of Washington State Muhammad Barik and Jennifer.
Climate Sensitivity Succession Regime Shifts Integration Current Proposal: The Dynamics of Change Next Proposal (due in < 4 years!!) Human Dimensions K-12.
Eco-System Services. The concept of Ecosystem Services has developed gradually for over a century as a way of recognizing the dependence of human societies.
Climate Change Adaptation Indicators. Adaptation Indicators- Origin and Purpose Adaptation Indicators.
RACC High School Training June 26, 2012 Jody Stryker University of Vermont Introduction to Watershed Hydrology.
Amazon Basin Revision AS 2.1 Natural Landscapes AS 2.1.
VCE Geography Unit 1: Natural Environments. Overview This unit investigates the geographic characteristics of natural environments and the natural processes.
Physical and Human Geography
Predicting the hydrologic implications of land use change in forested catchments Dennis P. Lettenmaier Department of Civil and Environmental Engineering.
Climate Smart Agricultural Development in the Goulburn Broken A regional climate change adaptation partnership project.
Climate Smart Agricultural Development in the Goulburn Broken
Community Land Model (CLM)
Fundamentals of River Restoration and Salmonid Fisheries OWEB, 1999, Fundamentals of River Restoration and Salmonid Fisheries Dylan Castle.
CEE6400 Physical Hydrology
Precipitation-Runoff Modeling System (PRMS)
Overview and Background of the Multi-scale Integrated Model of Ecosystem Services ( MIMES) Roelof Boumans February 2016 LABELS ON THE SLIDE?
Reading: Applied Hydrology Sections 5.1 and 5.2
Proposed CSES research in hydrology and water resources
Constructive and Destructive Processes
Climate Smart Agricultural Development in the Goulburn Broken
Environmental modeling application domains
Hydrologic Modeling in GCIP and GAPP
Workshop on hyper-resolution land surface modeling
Hydrology and Meteorology: A Symbiotic Relationship
Presentation transcript:

Vegetation & Landscape Questions: Predict interactions hydrology, vegetation, land use, hydraulics (gH20 & surface) of floodplains. – Ex: Rio Puerco, NM: grazing, incision, aridification Predict Human effects on erosion, sediment delivery & storage. – Ex: Le Sueur River, MN: post-glacial incision, agriculture Predict effects of changing forestry practices, climate change, etc., on sediment production,delivery, storage, etc., and effects on fisheries in the mountains. – Ex: Oregon Coast Range: timber, landslides, salmon Predict interactions hydrology, vegetation, land use, hydraulics (gH20 & surface) of floodplains – Ex: Rio Puerco, NM: grazing, incision, aridification Generalize models developed for specific places?

Vegetation & Landscape Couplings: Vegetation ↔geomorphology/sediment/hydrology – Roughness – Cohesion – Hydrology (ET, runoff, interception) – Impoundment/trapping, storage – Soil production/weathering Human ↔ etc. – Economic ↔ management style: flow of biomass – Productivity: management style – Sociological: restoration opportunities Reservoirs…elephant in the room

Models, Gaps Time and space scales: – Event – Engineering (human, decadal to century) – Landform What do we need & what can we get from – Vegetation models – Human models What can we get from new data (e.g., hi-res topo)? Sensitivity to temporal & spatial resolutions? What do geomorphic models need to do to incorporate vegetation effects? [model elephant in the room: CHILD]