This data set contains sublimation rate data from laboratory studies of snow. Parameters include flow rate, measured sublimation rate, and theoretical maximum sublimation rate. Data were collected in cold rooms at the Cold Regions Research and Engineering Laboratory (CRREL), in Hanover, NH, during 2005 and 2006. The data were collected as part of a collaborative research project. The project aims to develop a quantitative understanding of the processes active in isotopic exchange between snow/firn and water vapor, which is important to Antarctic ice core interpretation.
Data are available via FTP in Microsoft Excel (.xls) format.
The following example shows how to cite the use of this data set in a publication. For more information, see our Use and Copyright Web page.
The following example shows how to cite the use of this data set in a publication. List the principal investigators, year of data set release, data set title, publisher: NSIDC, and digital media.
Neumann, Thomas A. 2009. Collaborative Research: Laboratory Studies of Isotopic Exchange in Snow. Boulder, Colorado USA: National Snow and Ice Data Center. http://dx.doi.org/10.7265/N51834DX.
| Category | Description |
|---|---|
| Data format | Microsoft Excel Spreadsheet (.xls) |
| Spatial coverage and resolution |
Southernmost Latitude: 43°N Northernmost Latitude: 43°N Westernmost Longitude: 72°W Easternmost Longitude: 72°W |
| Temporal coverage and resolution | Data were collected in 2005 and 2006. |
| File naming convention | sub_rate_data.xls |
| File size | The data file is 32 KB. |
| Parameter(s) | Flow Rate Measured Sublimation Rate Theoretical Maximum Sublimation Rate |
| Procedures for obtaining data | Data are available via FTP. |
Dr. Thomas Neumann
Cryospheric Sciences Branch
NASA Goddard Space Flight Center
Greenbelt, MD 20770
NSIDC User Services
National Snow and Ice Data Center
CIRES, 449 UCB
University of Colorado
Boulder, CO 80309-0449 USA
phone: +1 303.492.6199
fax: +1 303.492.2468
form: Contact NSIDC User Services
e-mail: nsidc@nsidc.org
This research was supported by National Science Foundation (NSF) Office of Polar Programs (OPP) grant number 0338008.
Data are in Microsoft Excel (.xls) format.
Data are available on the FTP site in the ftp://sidads.colorado.edu/pub/DATASETS/AGDC/neumann_nsidc_0445/ directory. The data set consists of one Microsoft Excel spreadsheet, sub_rate_data.xls.
The file, sub_rate_data.xls contains laboratory measurement data of snow sublimation rates.
The data set is 32 KB.
Snow was collected outdoors, and processed in the Cold Regions Research and Engineering Laboratory in Hanover, New Hampshire, USA.
Southernmost Latitude: 43°N
Northernmost Latitude: 43°N
Westernmost Longitude: 72°W
Easternmost Longitude: 72°W
Data were collected in 2005 and 2006.
This data set contains snow sublimation rate data, measured under specified temperatures in a laboratory setting.
| Parameter | Description |
|---|---|
| Flow rate (SLPM) | Measured flow rate in standard liters per minute |
| Measured sublimation rate | Measured sublimation rate in kilograms per second |
| Theoretical maximum sublimation rate | Theoretical maximum sublimation rate, in kg per second |
| Mass-transfer coefficient | Mass-transfer coefficient (meters per second) was calculated as a function of Reynolds Number. |
| Sublimation Rate Data | |||||||
| T = -5C | flow rate (SLPM) | 9.64E-01 | 1.76E+00 | 3.69E+00 | 8.12E+00 | ||
| measured sublimation rate | 5.12E-08 | 8.87E-08 | 1.64E-07 | 3.26E-07 | |||
| theoretical maximum sublimation rate | 5.64E-08 | 9.43E-08 | 1.82E-07 | 3.79E-07 | |||
Data are available via FTP.
The data set is 32 KB.
Data are accessible using spreadsheet software.
Data consists of sublimation rate measurements at a specified, fixed temperature. Samples consisted of approximately 100-gram sieved snow samples of a specific grain radius that had dry air drawn through them at specified flow rates. Measured flow rates were compared with theoretical maximum sublimation rates to assess the degree to which equilibrium was achieved. The mass transfer coefficient was determined from the measured sublimation rates. These data are expressed as a function of Reynolds number, and are provided in the spreadsheet.
For details of laboratory setup and instrumentation, see Neumann et. al., 2009.
The Mass-transfer coefficient (hm) was derived as a function of Reynolds Number (Re). Calculations were done assuming all sublimation happens in approximately 4 mm of the sample thickness. Other values of hm for 1 mm and 1 cm are given in Neumann et. al., 2009.
Neumann, T. A., M. R. Albert, C. Engel, Z. Courville, and F. Perron. 2009. A Revised Method of Calculating Snow Sublimation Rate Based on Laboratory Experiments and Mass-Transfer Theory. International Journal of Heat and Mass Transfer, 52, 309-315.
Neumann, T. A., M. R. Albert, R. Lomonaco, C. Engel, Z. Courville, F. Perron. 2008. Experimental Determination of Snow Sublimation Rate and Stable Isotopic Exchange. Annals of Glaciology, v.49, 1-6.
The following related documents are available on the NSIDC Web site:
| Document | Description | URL |
|---|---|---|
| Antarctic Glaciological Data Center | Data Center Web site | http://nsidc.org/agdc/ |
The following acronyms are used in this document.
| Acronym | Description |
|---|---|
| FTP | File Transfer Protocol |
| HM | Mass-transfer coefficent |
| NSIDC | National Snow and Ice Data Center |
| URL | Uniform Resource Locator |
| RE | Reynold's Number |
| .XLS | Microsoft Excel File Format |
4 January 2010
http://nsidc.org/data/docs/agdc/nsidc0445_neumann/index.html