Table of Contents
This page describes the SNODAS Tools input data in detail.
- SNODAS Data Grids
- Difference between SNODAS and SNOTEL Data
- Input Zone Dataset: Watershed Basins
- Colorado Basins
SNODAS Data Grids
The Snow Data Assimilation System (SNODAS) Data Products are hosted by the National Snow and Ice Data Center (NSIDC) and developed by the NOAA National Weather Service’s National Operational Hydrologic Remote Sensing Center (NOHRSC). SNODAS is a modeling and assimilation system providing estimates of snow cover variables for the purpose of hydrological modeling and analysis. For the purpose of this documentation, the relevant information regarding this specific project will be explained. All this information and more is described in detail at http://nsidc.org/data/docs/noaa/g02158_snodas_snow_cover_model/.
NOHRSC creates multiple national SNODAS raster grids each day.
that are produced daily:
|Snow Water Equivalent (SWE)|
|Snow Melt Runoff at the Base of snowpack|
|Sublimation from the snowpack|
|Sublimation of Blowing Snow|
|snowpack Average Temperature|
For the purpose of this project, the only parameter of interest is Snow Water Equivalent (SWE). The daily SWE grid values are snapshots of SWE for a specific date at 6:00 AM UTC (11:00 PM previous day MST). Below is an image of a daily SNODAS grid representing SWE values across the nation. The areas of higher SWE are represented by blue while the areas with lower or no SWE values are represented by brown.
SNODAS Snow Water Equivalent Masked Grid for January 16th, 2017 (6:00 AM UTC)
The SNODAS data is available in 2 spatial coverages: masked and unmasked data. The masked data is clipped to the contiguous US while the unmasked data extends to cover a larger area (see the table below). For the purpose of this project, the masked data is the more appropriate size and is the chosen avenue for data assimilation.
|Masked SNODAS Data||Unmasked SNODAS Data|
|Spatial Coverage||Contiguous U.S.||Southernmost Latitude: 24.0996 ° N, Northernmost Latitude: 58.2329 ° N, Westernmost Longitude: 130.5171 ° W, Easternmost Longitude: 62.2504 ° W|
|Spatial Resolution||30 arc seconds, nominally 1 km on the ground||30 arc seconds, nominally 1 km on the ground|
|Temporal Coverage||30 September 2003 to present||09 December 2009 to present|
|Temporal Resolution||24-hour, snapshot at 6:00 AM UTC||24-hour, snapshot at 6:00 AM UTC|
|Grid size||6,935 columns by 3,351 rows||8,192 columns by 4,096 rows|
|Grid values||16-bit, signed integers||16-bit, signed integers|
The temporal coverage of the masked data begins on September 30, 2003 and extends to the current date. For the purpose of this project, all available data files are downloaded starting on September 30, 2003.
The daily SNODAS datasets are stored in the following FTP site: ftp://sidads.colorado.edu under the pathname
This directory contains folders indicating the years of which the data temporally covers.
In each year’s folder, there are folders indicating each month of the year.
The 8 daily rasters representing each unique snowpack parameter are stored within zipped daily .tar files located in each specific month. The .tar files follow the
naming convention of
SNODAS_YYYYMMDD.tar where YYYYMMDD represents the date of SNODAS data.
Difference between SNODAS and SNOTEL Data
TODO smalers 2016-12-10 explain the difference between SNODAS and SNOTEL data
- provide SNODAS resources and links and explain generally what SNODAS is, as well as benefits and limitations, mention that SNODAS is distributed whereas SNOTEL and snow course are measurements at sites. Note that people want to correlate SNOTEL with SNODAS but that can be difficult. Explain how SNODAS model and data file format has changed over time and this project converts to consistent format. This project does the intersection with basin data because the SNODAS basins changed over time - see original proposal language. Split into sections as appropriate.
Input Zone Dataset: Watershed Basins
The SNODAS Tools calculate zonal snowpack statistics on the SNODAS SWE daily grids. Zonal statistics are statistics calculated by zone where the zones are defined by an input zone dataset and the values are defined by a raster grid. The raster grid is the daily SNODAS SWE grid. The input zone dataset is a watershed basin boundary shapefile where each feature represents a basin area of interest. One set of daily snowpack statistics is calculated for each feature of the watershed basin boundary shapefile.
The SNODAS Tools were originally designed to calculate snowpack statistics of Colorado basins. The next section explains the specifications of the original Colorado watershed basin boundary shapefile.
Although specifically designed for the state of Colorado, the SNODAS Tools can calculate snowpack statistics for any watershed basin(s) as long as the extent of the watershed basin boundary shapefile is contained within the bounds of the unmasked SNODAS grids.
The Colorado watershed basin boundary shapefile was developed by merging basin shapefiles provided by the following four National Weather Service (NWS) River Forecast Centers, as well as data from Northern Colorado Water Conservancy District.
Displayed below in green, the Colorado watershed basin boundary shapefile contains a total of 322 basins each with a unique id (LOCAL_ID). Right-click on the image and click Open image in new tab to see a larger view.
The Colorado watershed basin boundary shapefile displayed in green. The Colorado state boundary is drawn with a thick, black border.
Additional Details about the Colorado Basins
Local versus Total Basins
TODO smalers 2016-12-11 Smaller basins are aggregated to larger totals. Elevation zones are used in the basins included in the Northern Colorado Water Conservancy District boundary (Upper Colorado and Poudre Basins), and are also accumulated to produce a total for a basin. Provide a screen shot. Include information about watershed connectivity file and about the elevation zones.
Edits made to the Original Data Sources
As mentioned above, the Colorado watershed basin boundary shapefile was developed by merging basins from multiple
sources. The field
POLY_SOURC within the attribute table of the downloadable
Final Colorado Watershed Basin Input Shapefile
is designed to inform the user the originating source of each feature.
The majority of features within the Colorado watershed basin boundary shapefile were unchanged for the SNODAS Tools project. However, in the rare case, the boundary of a feature was edited to maintain integrity of the output products.
TODO egiles 03/27/17 Explain why the edits were made.
EDIT_FLAG within the attribute table of the downloadable
Final Colorado Watershed Basin Input Shapefile is designed to
track the basin features that have been edited from their original source for the SNODAS Tools project. A feature has been edited
from its original source if the value '1' is assigned to the
Available Colorado Basin Boundary Layers for Download
The Colorado watershed basin shapefile, as well as the original source data files, are available for download below:
|Layer||File Format||Download Link|
|Final Colorado Watershed Basin Input||Shapefile (.zip)||Final CO Watershed Basin Shapefile|
|Final Colorado Watershed Basin Input||.GeoJSON||Final CO Watershed Basin GeoJSON|
|Original Basin Layer - ABRFC||Shapefile (.tar.gz)||Original Basin Layer - ABRFC|
|Original Basin Layer - CBRFC||Shapefile (.tar.gz)||Original Basin Layer - CBRFC|
|Original Basin Layer - MBRFC||Shapefile (.tar.gz)||Original Basin Layer - MBRFC|
|Original Basin Layer - WGRFC||-||-|
|Original Basin Layer - Northern Water||-||-|
|Input CO Basin Connectivity||.xlsx||Input CO Basin Connectivity .xlsx|
TODO egiles 03/27/17 ask Steve what to include about basin connectivity worksheet/basin list Excel file
TODO egiles 03/27/17 ask Steve if we should host the emailed shapefiles (Northern Water and WGRFC) on amazon services for download