Results 31 to 40 of about 1,329,248 (94)
The "tipping" temperature within Subglacial Lake Ellsworth, West Antarctica and its implications for lake access. [PDF]
We present results from new geophysical data allowing modelling of the water flow within Subglacial Lake Ellsworth (SLE), West Antarctica. Our simulations indicate that this lake has a novel temperature distribution due to significantly thinner ice than ...
Woodward, J. +19 more
core +2 more sources
Comparison of Lake Ice Extraction Methods Based on MODIS Images
As an important part of the cryosphere, lake ice is a sensitive indicator of climate change. Remote sensing technology can quickly and accurately monitor the process of its formation and decay, among which Moderate Resolution Imaging Spectroradiometer ...
Hongfang Zhang +4 more
doaj +1 more source
Is Vostok lake in steady state? [PDF]
Stable-isotope (D and 18O) data from the Vostok (East Antarctica) ice core are used to explore whether or not subglacial Vostok lake is in isotopic steady state. A simple box model shows that the lake is likely to be in steady state on time-scales of the
Royston-Bishop, G +9 more
core +1 more source
Arctic lakes are sensitive to climate change, and the timing and duration of ice presence and absence (i.e., ice phenology) on the lake surface can be used as a climate indicator.
Samuel E. Tuttle +5 more
doaj +1 more source
Lake ice Phenology across Tibetan Plateau (TPLIP)
This is a long-term lake ice phenology (LIP) dataset of 132 lakes across the Tibetan Plateau during 1978-2016. The dataset was extracted from long-term daily-scale lake surface temperature series simulated by modified air2water model, while the model was
Bing Zhang (8747476) +5 more
core +1 more source
A stratigraphic link across 1100 km of the Antarctic Ice Sheet between the Vostok ice-core site and Titan Dome (near South Pole) [PDF]
Isochronous internal ice-sheet layering, measured from airborne 60 MHz radar, was traced between Lake Vostok and the Titan Ice Dome (100 km from South Pole Station), Antarctica. Three layers were selected between Ridge B and Titan Dome, and between Ridge
Siegert, MJ +3 more
core +1 more source
Lake ice is a dominant component of Canada’s landscape and can act as an indicator for how freshwater aquatic ecosystems are changing with warming climates.
Justin Murfitt, Claude R. Duguay
doaj +1 more source
(Table 3) Ice phenology characteristics during the freeze-up period at Great Bear Lake and Great Slave Lake ...
Claude R Duguay (6967259) +5 more
core +1 more source
(Table 4) Ice phenology characteristics during the break-up period at Great Bear Lake and Great Slave Lake ...
Claude R Duguay (6967259) +5 more
core +1 more source
Measurement(s) lake ice phenology Technology Type(s) remote sensing and numerical ...
Yanhong Wu +7 more
doaj +1 more source

