An elevation change dataset in Greenland ice sheet from 2003 to 2020 using satellite altimetry data

An elevation change dataset in Greenland ice sheet from 2003 to 2020 using satellite altimetry data


This dataset provided the long-term elevation change rates data of the GrIS in three different periods using the ICESat data (February 2003 to October 2009), the Cryosat-2 data (August 2010 to October 2018) and the ICESat-2 data (October 2018 to December 2020) respectively. The dataset is named by the data.The data revealed that the elevation change rates of the GrIS were -12.19±3.81 cm/yr, -19.70±3.61 cm/yr and -23.39±3.06 cm/yr in the three different periods. In general, the obtained results agree with the trends discovered by other studies that were also derived from satellite altimetry data. This dataset provides the basic data for research into the impact of climate change over the GrIS.


File naming and required software

The dataset is named by the data. It contains three raster files and three shpfiles. The raster files are the interpolated 5 km×5 km elevation change rate of GrIS using ordinary kriging in Stereographic North Pole projection coordinate system (EPSG 3413). The Shpfiles are the uncertainty information. Each file contains three columns including Uncertain, calculated, interpolat. ‘Uncertain’ is the uncertainty of elevation change rate in each gird cell. ‘Calculated’ and ‘interpolat’ mean this gird cell is the calculated or interpolated one.


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Cite as:

Huang, H., Yang, B., Liang, S., Li, X. (2022). An elevation change dataset in Greenland ice sheet from 2003 to 2020 using satellite altimetry data. A Big Earth Data Platform for Three Poles, DOI: 10.11888/Cryos.tpdc.272758. CSTR: 18406.11.Cryos.tpdc.272758. (Download the reference: RIS | Bibtex )

Using this data, the data citation is required to be referenced and the related literatures are suggested to be cited.


References literature

1.Zwally, H.J., Schutz, R., Hancock, D., & Dimarzio, J. (2014). GLAS/ICESat L2 Global Antarctic and Greenland Ice Sheet Altimetry Data (HDF5), Version 34. [Indicate subset used]. Boulder, Colorado USA. NASA National Snow and Ice Data Center Distributed Active Archive Center. doi: https://doi.org/10.5067/ICESAT/GLAS/DATA209. (View Details )

2.Smith, B., Fricker, H. A., Gardner, A., Siegfried, M.R., Adusumilli, S., Csathó, B. M., Holschuh, N., Nilsson, J., Paolo, F.S., & the ICESat-2 Science Team. (2020). ATLAS/ICESat-2 L3A Land Ice Height, Version 3. [Indicate subset used]. Boulder, Colorado USA. NASA National Snow and Ice Data Center Distributed Active Archive Center. doi: https://doi.org/10.5067/ATLAS/ATL06.003. (View Details )

3.Krishfield, R., Kurtz, N., Farrell, S., & Davidson, M. (2013). CryoSat-2 estimates of Arctic sea ice thickness and volume, Geophysical Research Letters, 40, doi:10.1002/grl.50193. (View Details )


Support Program

CASEarth:Big Earth Data for Three Poles(grant No. XDA19070000) (No:XDA19000000)

Copyright & License

To respect the intellectual property rights, protect the rights of data authors, expand services of the data center, and evaluate the application potential of data, data users should clearly indicate the source of the data and the author of the data in the research results generated by using the data (including published papers, articles, data products, and unpublished research reports, data products and other results). For re-posting (second or multiple releases) data, the author must also indicate the source of the original data.


License: This work is licensed under an Attribution 4.0 International (CC BY 4.0)


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Keywords
Geographic coverage
East: 11.00 West: 73.00
South: 59.00 North: 83.00
Details
  • Temporal resolution: 1 year < x < 10 year
  • Spatial resolution: 1m - 10m
  • File size: 7 MB
  • Views: 181
  • Downloads: 4
  • Access: Open Access
  • Temporal coverage: 2003-02-01 To 2020-12-31
  • Updated time: 2022-08-16
Contacts
: HUANG Huabing    YANG Bojin    LIANG Shuang    LI Xinwu   

Distributor: A Big Earth Data Platform for Three Poles

Email: poles@itpcas.ac.cn

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