Zobrazeno 1 - 10
of 23
pro vyhledávání: '"D. J. Lampkin"'
Autor:
S. Eftekharzadeh Kay, B. N. Wenny, K. J. Thome, M. Yarahmadi, D. J. Lampkin, M. H. Tahersima, N. Voskanian
Publikováno v:
Remote Sensing, Vol 16, Iss 19, p 3588 (2024)
The two near-identical pushbroom Thermal Infrared Sensors (TIRS) aboard Landsat 8 and 9 are currently imaging the Earth’s surface at 10.9 and 12 microns from similar 705 km altitude, sun-synchronous polar orbits. This work validates the consistency
Externí odkaz:
https://doaj.org/article/be2b4f1d0f6d4a758e5fa29cba7ee747
Autor:
L. S. Koenig, D. J. Lampkin, L. N. Montgomery, S. L. Hamilton, J. B. Turrin, C. A. Joseph, S. E. Moutsafa, B. Panzer, K. A. Casey, J. D. Paden, C. Leuschen, P. Gogineni
Publikováno v:
The Cryosphere, Vol 9, Iss 4, Pp 1333-1342 (2015)
Increased surface melt over the Greenland Ice Sheet (GrIS) is now estimated to account for half or more of the ice sheet's total mass loss. Here, we show that some meltwater is stored, over winter, in buried supraglacial lakes. We use airborne radar
Externí odkaz:
https://doaj.org/article/5c82a88735fa4903a9f2b06b5cfafcd4
Publikováno v:
The Cryosphere, Vol 7, Iss 3, Pp 917-931 (2013)
Accumulated snow in the McMurdo Dry Valleys, while limited, has great ecological significance to subnivian soil environments. Though sublimation dominates the ablation process in this region, measurable increases in soil moisture and insulation from
Externí odkaz:
https://doaj.org/article/b40805a3253e417d9a10aac3c63ce1c8
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
Supraglacial lakes over the Greenland Ice Sheet can demonstrate multi-model drainage states. Lakes can demonstrate incomplete drainage, where residual melt can become buried under ice and snow and survive throughout the winter. We evaluate atmospheri
Publikováno v:
Frontiers in Earth Science, Vol 6 (2018)
The Greenland Ice Sheet has experienced accelerated mass loss over the last couple decades, in part due to destabilization of marine-terminating outlet glaciers. Retreat and acceleration of outlet glaciers coincides with atmospheric and oceanic warmi
Autor:
Casey Joseph, D. J. Lampkin
The impact of melt water injection into ice streams over the Greenland Ice Sheet is not well understood. Water-filled crevasses along the shear margins of Jakobshavn Isbræ are known to fill and drain, resulting in weakening of the shear margins due
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::edbfae8a76a38e54cb75630c3e8440b6
https://www.the-cryosphere-discuss.net/tc-2017-86/
https://www.the-cryosphere-discuss.net/tc-2017-86/
Publikováno v:
Antarctic Science. 27:197-209
Liquid water is scarce across the landscape of the McMurdo Dry Valleys (MDV), Antarctica, a 3800 km2ice-free region, and is chiefly associated with soils that are adjacent to streams and lakes (i.e. wetted margins) during the annual thaw season. Howe
Autor:
J. VanderBerg, D. J. Lampkin
Publikováno v:
Hydrological Processes. 28:6038-6053
Supraglacial channels are an important mechanism for surface water transport over the ablation zone of western Greenland. The first assessment of the spatio-temporal distribution of surface melt channels and their relationship to supraglacial lakes o
Autor:
D. J. Lampkin, U. Wade
Publikováno v:
International Journal of Remote Sensing. 34:6931-6946
This work evaluates the performance of an empirical inversion model for surface liquid water fraction LWF or melt magnitude, using data from the Moderate Resolution Imaging Spectroradiometer MODIS. Estimates of melt magnitude were evaluated through q
Autor:
Cristina D. Takacs-Vesbach, J. W. Eveland, D. J. Lampkin, Michael N. Gooseff, John E. Barrett
Publikováno v:
The Cryosphere, Vol 7, Iss 3, Pp 917-931 (2013)
Accumulated snow in the McMurdo Dry Valleys, while limited, has great ecological significance to subnivian soil environments. Though sublimation dominates the ablation process in this region, measurable increases in soil moisture and insulation from