by studying the layers of snowpack we can improve our predictions of when and where avalanches are...

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By studying the layers By studying the layers of snowpack we can of snowpack we can improve our predictions improve our predictions of when and where of when and where avalanches are likely to avalanches are likely to occur. occur. Note that Note that precipitation precipitation amounts seem to amounts seem to directly dictate directly dictate the discharge the discharge level. However, it level. However, it is important to is important to realize that 1997 realize that 1997 the Snake River the Snake River experienced more experienced more rainfall than rainfall than 1996; yet, 1996; yet, discharge for that discharge for that year fell below year fell below that of the 1996 that of the 1996 levels. This is levels. This is because the levels because the levels of discharge rely of discharge rely more heavily on more heavily on water from water from snowmelt. snowmelt. (3) California, Nevada, Oregon and Idaho all California, Nevada, Oregon and Idaho all fell under the ‘Above Average’ range for fell under the ‘Above Average’ range for potential flood risk. This was due to potential flood risk. This was due to persistent rainy conditions, as well as persistent rainy conditions, as well as increased snow melt due to an above average increased snow melt due to an above average snowpack in the mountains. When this snowpack in the mountains. When this assessment was issued there had already been assessment was issued there had already been reported flooding reported flooding in Sacramento in Sacramento and San Joaquin and San Joaquin River basins in River basins in central California. central California. (5) GIS and Snow Hydrology GIS and Snow Hydrology Why Study Snow? Why Study Snow? Water from snowmelt runoff is the main source of water supply for people living in various regions of the globe. Western Canada, Asia, India, and much of Rocky Mountain West in the US all rely upon the melt water. The water is used for, but not limited to: industry, electricity production, and irrigation. Melt water has an obvious influence on all of the surrounding ecosystems and their individual components. Both too much and too little snowmelt runoff can drastically affect a region. The negative effects of flooding and water shortages are not always preventable, but they can be predicted with the help of GIS and remote sensing technologies. This application can save lives and buy time for important preparation. A Work In A Work In Progress Progress Snow Runoff Model (SRM) WetSpa Model This particular model uses data from the land such as soil and elevation in a GIS in order to predict floods and allow for visualization of spatial distribution of hydrologic characteristics of a place. “The WetSpa model uses a modified rational method to calculate runoff and degree-day coefficient method to estimate the snow melt runoff based on temperature data” (1) . It does this by routing the runoff water across the geography of the low lying basin. By using a “diffusive wave transfer model” calculations can be made for the distance between any two points of water flow. It must take into account that these calculations will vary depending upon the different geographies of the basin. Sources: Sources: The version for Windows, WinSRM, is now available for public use. The SRM is a “degree-day model.” It needs input from remote sensing unit. tested globally for over 60 different basins, the SRM has been a success in both forecasts and simulations. To get outputs the model uses a collection of data from temperature, precipitation, and snow cover observations. Thus, “model parameters can either be derived from measurements or estimated by hydrological judgment taking into account the basin characteristics, physical laws, and theoretical or empirical relationships” (4) . "The one word of skepticism I have on these studies is that ultimately we are talking about modeling, and modeling just doesn't have a good track record for predicting the future.” (2) – Bonner Cohen, National Center for Public Policy (2005) As with any new application of technology, monitoring and analyzing the snowmelt is an ongoing learning process. Scientists are constantly evaluating and tweaking the current technologies in hopes of advancing in the future. QHM This model is for use by people who have a good understanding of hydrologic concepts. This model is particularly useful in applications for snow or ice hydrology. Input values in the QHM are region specific, as it takes into account the differences that are present from one climate zone to the next. This is a continuous simulation model and can even operate continuously for more than one project. 1.) A. Bahremand, J. Corluy, Y. Liu, F. De Smedt, J.Poorova, and L.Velcická. River Flow Simulation By WetSpa Model in Hornad Watershed,Slovakia. www.astro.oma.be/BNCGG/contactforum10_05/abstract-contrib/abstract14.doc. Accessed on January 25, 2007. 2.) Hall, Carl T. San Francisco Chronicle. Global Warming Study Forecasts More Water Shortages; Climate Change Already Affecting Sierra Snowpack. November 17, 2005. http://www.sfgate.com/cgibin/article.cgi?f=/c/a/2005/11/17/MNG4EFPHK51.DTL&type=science . Accessed on January 22, 2007. 3.) Lamar. Mike. Term Project - Snowpack Analysis Using GIS. http://www.crwr.utexas.edu/gis/gishydro01/Class/trmproj/lamar/termproject.html . Accessed on January 24, 2007. 4.) J. Martinec . A. Rango, R. Roberts. SRM User’s Manual (Abstract). http://hydrolab.arsusda.gov/~rroberts/srmmanual/srmman.html . Allison Hurley – Geog 36 Allison Hurley – Geog 363 We Use GIS Models to… - calculate snow depth - calculate snow depth - understand snowpack - understand snowpack composition composition - monitor snowcover and - monitor snowcover and compare to compare to previous observations previous observations - improve flood protection - improve flood protection In Order to… - predict the impact - predict the impact sediments sediments and pollutants in and pollutants in runoff will have runoff will have on waterways on waterways - understand and - understand and prepare for prepare for snow related snow related disasters disasters (i.e. avalanches) (i.e. avalanches) - detect changes in - detect changes in climate climate - predict future stress - predict future stress on the biota on the biota of a region of a region

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Page 1: By studying the layers of snowpack we can improve our predictions of when and where avalanches are likely to occur. Note that precipitation amounts seem

By studying the layers of By studying the layers of snowpack we can improve snowpack we can improve our predictions of when and our predictions of when and where avalanches are likely where avalanches are likely to occur. to occur.

Note that Note that precipitation amounts precipitation amounts seem to directly seem to directly dictate the discharge dictate the discharge level. However, it is level. However, it is important to realize important to realize that 1997 the Snake that 1997 the Snake River experienced River experienced more rainfall than more rainfall than 1996; yet, discharge 1996; yet, discharge for that year fell for that year fell below that of the below that of the 1996 levels. This is 1996 levels. This is because the levels of because the levels of discharge rely more discharge rely more heavily on water from heavily on water from snowmelt.snowmelt. (3)

California, Nevada, Oregon and Idaho all fell under California, Nevada, Oregon and Idaho all fell under the ‘Above Average’ range for potential flood risk. the ‘Above Average’ range for potential flood risk. This was due to persistent rainy conditions, as well This was due to persistent rainy conditions, as well as increased snow melt due to an above average as increased snow melt due to an above average snowpack in the mountains. When this assessment snowpack in the mountains. When this assessment was issued there had already been reported floodingwas issued there had already been reported floodingin Sacramento in Sacramento and San Joaquinand San JoaquinRiver basins in River basins in central California.central California. (5)

GIS and Snow HydrologyGIS and Snow HydrologyWhy Study Snow?Why Study Snow?

Water from snowmelt runoff is the main source of water supply for people living in various regions of the globe. Western Canada, Asia, India, and much of Rocky Mountain West in the US all rely upon the melt water.

The water is used for, but not limited to: industry, electricity production, and irrigation. Melt water has an obvious influence on all of the surrounding ecosystems and their individual components.

Both too much and too little snowmelt runoff can drastically affect a region. The negative effects of flooding and water shortages are not always preventable, but they can be predicted with the help of GIS and remote sensing technologies. This application can save lives and buy time for important preparation.

A Work In A Work In ProgressProgress

Snow Runoff Model (SRM) WetSpa Model

This particular model uses data from the land such as soil and elevation in a GIS in order to predict floods and allow for visualization of spatial distribution of hydrologic characteristics of a place. “The WetSpa model uses a modified rational method to calculate runoff and degree-day coefficient method to estimate the snow melt runoff based on temperature data”(1). It does this by routing the runoff water across the geography of the low lying basin. By using a “diffusive wave transfer model” calculations can be made for the distance between any two points of water flow. It must take into account that these calculations will vary depending upon the different geographies of the basin.

Sources:Sources:

The version for Windows, WinSRM, is now available for public use. The SRM is a “degree-day model.” It needs input from remote sensing unit. tested globally for over 60 different basins, the SRM has been a success in both forecasts and simulations. To get outputs the model uses a collection of data from temperature, precipitation, and snow cover observations. Thus, “model parameters can either be derived from measurements or estimated by hydrological judgment taking into account the basin characteristics, physical laws, and theoretical or empirical relationships”(4).

"The one word of skepticism I have on these studies is that ultimately we are talking about modeling, and modeling just doesn't have a good track record for predicting the future.” (2) – Bonner Cohen, National Center for Public Policy (2005)

As with any new application of technology, monitoring and analyzing the snowmelt is an ongoing learning process. Scientists are constantly evaluating and tweaking the current technologies in hopes of advancing in the future.

QHM

This model is for use by people who have a good understanding of hydrologic concepts. This model is particularly useful in applications for snow or ice hydrology. Input values in the QHM are region specific, as it takes into account the differences that are present from one climate zone to the next. This is a continuous simulation model and caneven operate continuously for more than one project.

1.) A. Bahremand, J. Corluy, Y. Liu, F. De Smedt, J.Poorova, and L.Velcická. River Flow Simulation By WetSpa Model in Hornad Watershed,Slovakia. www.astro.oma.be/BNCGG/contactforum10_05/abstract-contrib/abstract14.doc. Accessed on January 25, 2007. 2.) Hall, Carl T. San Francisco Chronicle. Global Warming Study Forecasts More Water Shortages; Climate Change Already Affecting Sierra Snowpack. November 17, 2005. http://www.sfgate.com/cgibin/article.cgi?f=/c/a/2005/11/17/MNG4EFPHK51.DTL&type=science. Accessed on January 22, 2007.3.) Lamar. Mike. Term Project - Snowpack Analysis Using GIS. http://www.crwr.utexas.edu/gis/gishydro01/Class/trmproj/lamar/termproject.html. Accessed on January 24, 2007.4.) J. Martinec . A. Rango, R. Roberts. SRM User’s Manual (Abstract). http://hydrolab.arsusda.gov/~rroberts/srmmanual/srmman.html. Accessed on January 22, 2007.5.) National Weather Service - Hydrologic Information Center. 2006 National Hydrologic Assessment. Elevated Flood Risk in Parts of West and Mid-West. April 14, 2006. http://www.nws.noaa.gov/oh/hic/nho/. Accessed on January 25, 2007.

Allison Hurley – Geog 363: Section 006Allison Hurley – Geog 363: Section 006

We Use GIS Models to… - calculate snow depth- calculate snow depth - understand snowpack composition - understand snowpack composition - monitor snowcover and compare - monitor snowcover and compare toto previous observations previous observations - improve flood protection - improve flood protection

In Order to… - predict the impact - predict the impact sediments sediments and pollutants in runoff will and pollutants in runoff will have have on waterways on waterways - understand and prepare for - understand and prepare for snow related disasters snow related disasters (i.e. avalanches) (i.e. avalanches) - detect changes in climate - detect changes in climate - predict future stress on the - predict future stress on the biota biota of a region of a region

Page 2: By studying the layers of snowpack we can improve our predictions of when and where avalanches are likely to occur. Note that precipitation amounts seem