Data Set ID:
ASO_50M_SWE

ASO L4 Lidar Snow Water Equivalent 50m UTM Grid, Version 1

This data set contains 50 m gridded snow water equivalent (SWE) values collected as part of the NASA/JPL Airborne Snow Observatory (ASO) aircraft survey campaigns. The data were derived from the ASO L4 Lidar Snow Depth 50m UTM Grid data product and from modeled snow density.

This is the most recent version of these data.

Version Summary:

Initial release

STANDARD Level of Service

Data: Data integrity and usability verified

Documentation: Key metadata and user guide available

User Support: Assistance with data access and usage; guidance on use of data in tools

See All Level of Service Details

Parameter(s):
  • SNOW/ICE > SNOW WATER EQUIVALENT
Data Format(s):
  • GeoTIFF
Spatial Coverage:
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Platform(s):DHC-6, King Air
Spatial Resolution:
  • 50 m x 50 m
Sensor(s):Riegl LMS-Q1560
Temporal Coverage:
  • 3 April 2013 to 2 June 2018
Version(s):V1
Temporal ResolutionVariesMetadata XML:View Metadata Record
Data Contributor(s):Thomas Painter

Geographic Coverage

Other Access Options

Other Access Options

Close

As a condition of using these data, you must cite the use of this data set using the following citation. For more information, see our Use and Copyright Web page.

Painter, T. 2018. ASO L4 Lidar Snow Water Equivalent 50m UTM Grid, Version 1. [Indicate subset used]. Boulder, Colorado USA. NASA National Snow and Ice Data Center Distributed Active Archive Center. doi: https://doi.org/10.5067/M4TUH28NHL4Z. [Date Accessed].
Created: 
23 May 2018
Last modified: 
17 July 2019

Data Description

This data set is a collection of 50 m resolution snow water equivalent (SWE) maps, measured by the Airborne Snow Observatory (ASO), a coupled imaging spectrometer and scanning lidar system created by NASA/JPL. The imaging spectrometer is used to quantify spectral albedo, broadband albedo, and radiative forcing by dust and black carbon in snow. The scanning lidar measures snow depth using the differential altimetry approach of subtracting snow-free gridded elevation data from snow-covered gridded elevation data (Deems et al., 2013). The original 3 m snow depth measurements, which are provided in the ASO L4 Lidar Snow Depth 3m UTM Grid data set, were used to aggregate the 50 m gridded snow depth data in the ASO L4 Lidar Snow Depth 50m UTM Grid data set. To infer the SWE data presented here, the 50 m snow depth data were combined with snow density modeled by iSnobal, a raster-distributed, physically-based energy-balance model.

Parameters

Parameter Description

The data product featured in this data set is SWE in meters. An example is shown in Figure 1.

Sample Data Record

Figure 1. SWE (in meters) in the Tuolumne Basin, California, on 26 April 2016. Image courtesy of NASA/JPL Airborne Snow Observatory.

File Information

Format

Data are provided as GeoTIFF (.tif) formatted files. Each GeoTIFF file is paired with an associated XML file, which contains additional metadata.

Naming Convention

Data files are named after the following naming convention and as described in Table 1.

ASO_50M_SWE_CCSCBC_YYYMMDD.tif

Example file name:

ASO_50M_SWE_USWAOL_20160208.tif

File Designator Description
Table 1. File Naming Convention
ASO_50M_SWE ASO L4 Lidar Snow Water Equivalent 50 m UTM Grid product short name
CC Two digit country code, e.g. US = United States
SC Two digit US state code, e.g. WA = Washington
BC Two digit basin (site) code, e.g. OL = Olympic Mountains. See the ASO basins spreadsheet for a list of basins and basin codes.
YYYYMMDD Data acquisition date
.tif GeoTIFF formatted file

File Size

The total data file volume is approximately 338 MB.

Spatial Information

Coverage

Spatial coverage for this data set includes several basins listed in the ASO basins spreadsheet. Figure 2 depicts four California basins as an example.

Figure 2. ASO California basins: Tuolumne Basin (red), Merced Basin (blue), Lake Basin (orange), and Kings Basin (green). Image courtesy of NASA/JPL Airborne Snow Observatory.
Note: At this point, not all the basins listed in the ASO basins spreadsheet are provided in this data set. More basins will be added as this data set grows.

Resolution

50 m x 50 m grid

Geolocation

  • Datum: WGS84 Ellipsoidal
  • UTM zones: 10N, 11N, 12N, 13N 
  • EPSG codes: 32610, 32611, 32612, 32613

Temporal Information

Coverage

03 April 2013 to 02 June 2018

ASO Snow-Off campaigns typically occur between August and October, while the Snow-On campaigns are typically conducted between February and June.

Resolution

Varies by seasonal campaigns. In general, given the rapidly changing nature of snow cover presence, depth, and surface properties that modulate its melt, ASO flies target basins on a weekly basis from mid-winter through complete snowmelt.

Data Acquisition and Processing

Processing Steps

The reader is referred to Painter et al. (2016) for details on the processing steps used to generate these data.

Quality, Errors, and Limitations

The reader is referred to Painter et al. (2016) for more information on the quality of the data.

Instrumentation

Lidar System

The Riegl LMS-Q1560 airborne laser scanner (ALS) measures surface elevations, from which snow depths are calculated. The Q1560 uses dual lasers at 1064 nm wavelength, each with a 60° scan angle (±30° across-nadir) and a 14° angle relative to the cross-track axis, producing an up to 8° fore/aft look angle (off-nadir in the along-track direction). A 1064 nm wavelength system is used because of its relatively small laser penetration depth in snow and relatively high snow reflectance at that wavelength, as well as greater penetration through vegetation canopies.

Note: Current processing uses some data from the CASI 1500 imaging spectrometer data to discriminate processing steps, but the bulk of the snow depth information, from which the SWE data are derived, comes from the Riegl Q1560 airborne laser scanner.

The required level of geolocation accuracy is achieved through the use of a single lidar-integrated Trimble Applanix POS/AV 510 GPS and Inertial Measurement Unit (IMU). The IMU has angular uncertainties of 0.005° in roll, 0.005° in pitch, and 0.008° in true heading after post-processing, and a resultant attitude uncertainty of 0.011°.

For more detailed information see Deems et al. (2013) and Painter et al. (2016).

Software and Tools

Software that recognizes the GeoTIFF file format is recommended for these images, such as the GIS software QGIS and ArcGIS. See also the libGeoTIFF and GDAL websites for more information.

Related Data Sets

Related Websites

Contacts and Acknowledgments

Thomas Painter
Jet Propulsion Laboratory
4800 Oak Grove Drive
Pasadena, CA 91109

Acknowledgments

Funding for the Airborne Snow Observatory was provided by NASA, the California Department of Water Resources, JPL investments, Colorado Water Conservation Board, City of San Francisco Public Utilities Commission, Turlock Irrigation District, Modesto Irrigation District, and USDA Agricultural Research Service.

References

Deems, J. S., Painter, T. H., & Finnegan, D. C. (2013). Lidar measurement of snow depth: a review. Journal of Glaciology, 59(215), 467–479. https://doi.org/10.3189/2013jog12j154

Painter, T. H., Berisford, D. F., Boardman, J. W., Bormann, K. J., Deems, J. S., Gehrke, F., … Winstral, A. (2016). The Airborne Snow Observatory: Fusion of scanning lidar, imaging spectrometer, and physically-based modeling for mapping snow water equivalent and snow albedo. Remote Sensing of Environment, 184, 139–152. https://doi.org/10.1016/j.rse.2016.06.018

How To

Programmatically access data using spatial and temporal filters
The Common Metadata Repository (CMR) is a high-performance metadata system that provides search capabilities for data at NSIDC. A synchronous REST interface was developed which utilizes the CMR API, allowing you to ... read more