Zobrazeno 1 - 10
of 14
pro vyhledávání: '"JACK L. SABA"'
Publikováno v:
Journal of Glaciology, Vol 62, Pp 993-995 (2016)
Externí odkaz:
https://doaj.org/article/b1b4b0198f23497ba20440f3dc2a2bfb
Publikováno v:
Journal of Glaciology, Vol 62, Pp 990-992 (2016)
Externí odkaz:
https://doaj.org/article/cdff795424184690a0b0d329d895fbd2
Autor:
Jan F. McGarry, Claudia C. Carabajal, Joseph-Paul A Swinski, Stephen P. Palm, James E. Golder, Peter Liiva, Ann R Reese, Jack L. Saba, Stephen T Holland
Publikováno v:
Earth and Space Science, Vol 8, Iss 4, Pp n/a-n/a (2021)
Earth and Space Science (Hoboken, N.j.)
Earth and Space Science (Hoboken, N.j.)
The Advanced Topographic Laser Altimetry System (ATLAS) is the sole instrument on the Ice, Cloud, and land Elevation Satellite 2 (ICESat‐2). Without some method of reducing the transmitted data, the volume of ATLAS telemetry would far exceed the no
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::643f0bbeeb6d99a04c737204e87126e0
https://doaj.org/article/b358c8d35ed640679ba542430898f361
https://doaj.org/article/b358c8d35ed640679ba542430898f361
Publikováno v:
IEEE Transactions on Geoscience and Remote Sensing. 53:2011-2020
The Ice, Cloud, and land Elevation Satellite-2 (ICESat-2), the successor mission to ICESat, is planned to launch in 2017. The ICESat-2 spacecraft will carry the Advanced Topographic Laser Altimeter System (ATLAS). ATLAS will be the most precise space
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::108efab1e6646ba79a01389a0360740a
https://doi.org/10.1109/tgrs.2014.2352277
https://doi.org/10.1109/tgrs.2014.2352277
Publikováno v:
Journal of Glaciology. 61:1019-1036
Mass changes of the Antarctic ice sheet impact sea-level rise as climate changes, but recent rates have been uncertain. Ice, Cloud and land Elevation Satellite (ICESat) data (2003–08) show mass gains from snow accumulation exceeded discharge losses
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ac9a6b0366cf5d6fa9a61426ff6ab065
https://doi.org/10.3189/2015jog15j071
https://doi.org/10.3189/2015jog15j071
Publikováno v:
Journal of Glaciology. 62:990-992
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bab3fc54c41df0a21bc9e0c25a574e73
https://doi.org/10.1017/jog.2016.91
https://doi.org/10.1017/jog.2016.91
Publikováno v:
Journal of Glaciology. 62:993-995
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63dd04d3feaf548a0d2dafe0704134c6
https://doi.org/10.1017/jog.2016.92
https://doi.org/10.1017/jog.2016.92
Autor:
H. Jay Zwally, Jun Li, Anita C. Brenner, Matthew Beckley, Helen G. Cornejo, John DiMarzio, Mario B. Giovinetto, Thomas A. Neumann, John Robbins, Jack L. Saba, Donghui Yi, Weili Wang
Publikováno v:
Journal of Glaciology. 57:88-102
We derive mass changes of the Greenland ice sheet (GIS) for 2003–07 from ICESat laser altimetry and compare them with results for 1992–2002 from ERS radar and airborne laser altimetry. The GIS continued to grow inland and thin at the margins duri
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::85a05c69f424890a37343f984337b245
https://doi.org/10.3189/002214311795306682
https://doi.org/10.3189/002214311795306682
Autor:
Helen G. Cornejo, Jun Li, H. Jay Zwally, Donghui Yi, Matthew Beckley, Jack L. Saba, Anita C. Brenner, Mario B. Giovinetto
Publikováno v:
Journal of Glaciology. 51:509-527
Changes in ice mass are estimated from elevation changes derived from 10.5 years (Greenland) and 9 years (Antarctica) of satellite radar altimetry data from the European Remote-sensing Satellites ERS-1 and -2. For the first time, the dH/dt values are
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ae6f6e106f6cdd251743173abbe6de38
https://doi.org/10.3189/172756505781829007
https://doi.org/10.3189/172756505781829007
Autor:
Kristine M. Larson, H. Jay Zwally, Waleed Abdalati, Thomas A. Herring, Jack L. Saba, Konrad Steffen
Publikováno v:
Science. 297:218-222
Ice flow at a location in the equilibrium zone of the west-central Greenland Ice Sheet accelerates above the midwinter average rate during periods of summer melting. The near coincidence of the ice acceleration with the duration of surface melting, f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::556ae4f102f1f0befd0fcca45d1bde6a
https://doi.org/10.1126/science.1072708
https://doi.org/10.1126/science.1072708