Some results of zero-order analysis Ellen Douglas, 6/10/03

Slides:



Advertisements
Similar presentations
To Next Slide Unit 1 Chapter 1 Lesson 2 Rivers Change the Land 20 Questions!
Advertisements

Global 2 R Regents Review Spring 2009
Spatial Analysis with ArcView: 2-D. –Calculating viewshed –Calculating line of sight –Add x and y coordinates –Deriving slope from surface data –Deriving.
Maps.
Relationships between Nighttime Imagery and Population Density for Hong Kong Qing Liu Paul C. Sutton Christopher D. Elvidge Asia Pacific Advanced Network.
Climate Research in Nepal Himalayas Saraju K. Baidya (Department of Hydrology & Meteorology) “Mountains, witnesses of global changes. Research in the Himalaya.
ASB/BNPP Pantropic Analysis Kate Sebastian IFPRI.
Standard watershed and stream delineation recipe - Vector stream (ex. NHD data) fusion into DEM raster (burning in) - Sink removal - Flow direction - Flow.
Why clip basins with lakes and reservoirs?  Flash floods do not occur in lakes and reservoirs.  Similar to the situation in coastal areas, basins extending.
Development of urban form on the flood prone in Thailand; the case of Chao Phraya River Basin Thongchai Roachanakanan, PhD Office of Climate Change Convention.
Watershed analysis in Guatemala Including collected and generated data for Guatemala as well as some basic regional statistics calculated for the 40 major.
2007 Indiana GIS Conference City of Bloomington Contour Update Project Laura Haley, GIS Manager
Application of GIS on Landslide Susceptibility and risk mapping
URBAN FLOODS IN GREECE Current situation and major research and development needs in Urban Flood Management Cost meeting, Warsaw, 29-31/5/2008 Vassilopoulos.
Population Maps of Latin America Glenn Hyman, Andy Nelson, German Lema International Center for Tropical Agriculture Cali, Colombia.
Population Distribution
By virtue of the sloping topography of the region and the quality of the soil, as well as its proximity to the Dead Sea fault, region is exposed to.
RIVERS AND ASSOCIATED LANDFORMS
Nam Songkhram model application and field work National consultation with TNMC 20th of April 2006, Bangkok MRCS WUP-FIN.
Manager: John Daneri Analyst: Kathleen Callahan Assistant Manager: Jacob Powell Analyst: Leah Gibson.
The earth at night Source:
NATHAN FOSTER WARM SEASON WORKSHOP 5/2/12 The Flash Flood Potential Index (FFPI) Project at BTV.
Global 2 R Regents Review Spring 2011 Geography Review.
Arctic Temperatization Arctic Temperatization : A Preliminary Study of Future Climate Impacts on Agricultural Opportunities in the Pan-Arctic Drainage.
Estimating Pollutant Loads Caroni River Bolivar, Venezuela Global Applications of GIS Technology Lee Sherman.
How to stratify watersheds? For the regional-scale studies we need to identify the upper / middle / lower regions of each watershed. There are many ways.
Climate Regions, Biomes and Tropical Climates By: Ashley Pham and Mariana Bengochea.
WUP-FIN training, 3-4 May, 2005, Bangkok Hydrological modelling of the Nam Songkhram watershed.
Outline of the training. 6 October 2005, TNMC, Bangkok.
Simulating Rainfall Extremes in South America: Sensitivity to remote and local forcing Anji Seth and Maisa Rojas International Research Institute for Climate.
River flow modeling of the Mekong River Basin A.W. Jayawardena Department of Civil Engineering The University of Hong Kong
Delineating population clusters Applying grid methods Niek van Leeuwen Statistics Netherlands
DAM BREAK RISK IN COLOMBIA A Geospatial Assessment of Population Vulnerability from Flood Inundation Eugene Derner, GEOG 594a Spring 2014.
Chaiwat Ekkawatpanit, Weerayuth Pratoomchai Department of Civil Engineering King Mongkut’s University of Technology Thonburi, Bangkok, Thailand Naota Hanasaki.
National Consultation with TNMC 3 May 2005, Bangkok WUP-FIN Phase II – Model development.
MODULE 1 Water Framework Directive, Relation of WFD with Daughter Directives, River Basin Management Planning, Water Bodies, Typology, Classification River.
ARC GIS IN THE SANTA RIVER BASIN IN PERU GIS in Water Resources Fall 2006 Professor: Dr. David Maidment Presented by Presented by Eusebio Ingol.
Climate Impacts on New Connected Infrastructure Vulnerabilities.
U.S. Department of the Interior U.S. Geological Survey Idaho District Office (208) Estimating Hydropower Potential Using EDNA Stage.
Luz Adriana Cuartas Pineda Javier Tomasella Carlos Nobre
Diurnal Cycle of Precipitation Based on CMORPH Vernon E. Kousky, John E. Janowiak and Robert Joyce Climate Prediction Center, NOAA.
Page 55 Homework: Enjoy your break Page 56 Monday, November 23, 2015 Tuesday, November 24, 2015 Modeling River Basins E.Q. – How can you determine how.
How vulnerable is the Lower Niger Delta to inundation from Sea Level Rise? ZAHRAH N. MUSA, IOANA POPESCU, ARTHUR MYNETT UNESCO-IHE, Institute for Water.
LO - To create a revision case study card for the Mozambique floods in the year 2000.
Geography Geography – the study of the Earth’s environment and how it shapes people’s lives and how Earth is shaped in turn by people’s activities Example.
Low-Density Urbanization and Critical Habitats
From Relative Sea Level Rise to Coastal Risk: Estimating Contemporary and Future Flood Risk in Deltas CSDMS 2016 Annual Meeting May 19, 2016 Zachary Tessler1,
Estimating Annual Sediment Yield and a Sediment Delivery Ratio for Red Creek, Utah and Wyoming Paul Grams Department of Geography and Earth Resources.
David G. Tarboton Utah State University Ude Shankar NIWA, New Zealand
Urbanization and Development: Is LAC Different from the Rest of the World? Mark Roberts (GSURR, World Bank), Brian Blankespoor (DEC-RG, World Bank),
Map-Based Flood Hydrology and Hydraulics
Hydrologic Considerations in Global Precipitation Mission Planning
STREAM NETWORK DELINEATION USING ARC HYDRO AND TauDEM: A comparison of approaches using The Upper Sevier and the Little Bear River Basins Alphonce C. Guzha.
Regional Development SOL # 4.
Ch. 13 Modern Earth Science p
Digital Elevation Models and Hydrology
Some Project Ideas Literature review of particular subjects – what is new since “Applied Hydrology” was originally published? What are the key papers in.
Global Hydrologic Data Development
Parallel Computation of River Basin Hydrologic Response Using DHM
ASIAN STUDIES A REVIEW.
GIS FOR HYDROLOGIC DATA DEVELOPMENT FOR DESIGN OF HIGHWAY DRAINAGE FACILITIES by Francisco Olivera and David Maidment Center for Research in Water Resources.
Hydrology.
Map 12b: Contemporary land cover – percent pasture per 0.5
Utilizing Automated Tools in ArcGIS
Profiling risk and sustainability in coastal deltas of the world
Digital Elevation Models and Hydrology
SUCH A DISASTER HOT SPOT?
Geog 380 Watershed Analysis Digital Terrain Analysis and Geomorphology
Geography of Latin America & the Caribbean Picture Dictionary
River Systems.
Presentation transcript:

Some results of zero-order analysis Ellen Douglas, 6/10/03 Methods (analyses at 6-min resolution except where noted): Aggregated Landscan 2000 population data: original at 1 km resolution Delineated floodplains: min slope < 0.0005 within 15 km of a river or drainage canal (criteria from previous work). Selected 30-min grids cells within pan-tropical domain that were classified as dissected terrain (Meybeck, Green and Vorosmarty, 2001. A new typology for mountains and other relief classes, Mountain Research and Development, 21 (1): 34-45.) This will highlight basins in which populations are potentially more vulnerable to major floods resulting from deforestation.

Estimate population potentially vulnerable to flooding Methods: Select total population with delineated floodplains Compute population density (pop/sq. km) (slides 6-9) Overlay population density in floodplains on map of basins with >25% area classified as highly dissected (slides 10-13). I am hypothesizing that basins with >25% of their area in high relief are more sensitive to changes in hydrology from deforestation. This means that basins in Central America and Southeast Asia are of particular concern. This hypothesis will be tested with the modeling exercise.

Estimate population potentially vulnerable to flooding In the next four slides, I’ve pointed out basins with >25% highly dissected area and with high population density at or near the mouth. These downstream populations have the potential to be greatly affected by upstream land use changes.

Magdelena Basin

Ganges Basin

Hong Basin Chao Phraya Basin Mekong Basin

Preliminary Conclusions A synoptic analysis, even at a relatively coarse resolution, allows us to compare geophysical and population attributes across the entire modeling domain. This helps us to focus our attention and test our hypotheses on basins that have the greatest potential for increased human vulnerability due to deforestation. From this analysis, it appears that southern Asia should be (and in fact is) our main focus due to high population densities within floodplains (esp near the river mouths) coupled with high relief basins.