Results 191 to 200 of about 2,868,735 (385)
Spectral curves of surface reflectance in some Antarctic regions [PDF]
Angelo Lupi +8 more
openalex
ABSTRACT This study examines the impact of geological, marine and anthropogenic sources on metal and metalloid concentrations in the forefields of four glaciers (Ecology, Sphinx, Tower and Windy) on King George Island, Antarctic. Water samples were collected at the beginning and end of the hydrological season (austral summer, December 2021 to February ...
Joanna Potapowicz +8 more
wiley +1 more source
Abstract Future precipitation projections rely heavily on climate models, underscoring the need to evaluate their ability to simulate historical precipitation changes. Using multiple atmospheric models and ensemble simulations, we estimate the forced signals driven by sea surface warming and the direct effects of greenhouse gases and aerosols, as well ...
Wengui Liang +5 more
wiley +1 more source
Continental outflow shapes the circum-Antarctic pattern of summertime atmospheric mercury depletion zones. [PDF]
Xie Z +7 more
europepmc +1 more source
A voyage of discovery and research in the southern and Antarctic regions, during the years 1839-43
J. Ross
semanticscholar +1 more source
Remote Sensing Sediment–Albedo Feedbacks Affecting Ice Thickness on Taylor Valley Lakes, Antarctica
Abstract The McMurdo Dry Valleys are the largest unglaciated region in Antarctica and home to perennially frozen lakes. Thirty years of ice thickness measurements reveal meter‐scale fluctuations over decadal time scales. In this paper, we hypothesize that changing surface sediment dynamics alter ice albedo, changing the heat balance and thickness of ...
C. E. Dougherty +4 more
wiley +1 more source
Quality over Quantity: Organic Compounds Altering the Antarctic Sea Spray Aerosol Concentrations. [PDF]
Dall'osto M +13 more
europepmc +1 more source
The Atmosphere's Substantial Role in Interannual Variability of Earth's Energy Imbalance
Abstract Earth's Energy Imbalance (EEI) is a key metric to quantify climate change. While the ocean absorbs most excess heat, the atmosphere contributes only 1%–2% to the long‐term mean of EEI. However, our analysis of observational data demonstrates that variations in the atmosphere's energy content play a much larger role in interannual variations of
Michael Mayer +4 more
wiley +1 more source

