Add to ORKGRadiative energy is critical in controlling the heat and mass balance of sea ice, which significantly affects the polar climate. In the polar oceans, light transmission through the atmosphere and sea ice is essential to th
The primary driver of the climate system is the uneven distribution of incoming and outgoing radiati...
Light (solar short-wave radiation) transmission into and through sea ice is of high importance for v...
The loss of Arctic sea ice has emerged as a leading signal of global warming. This, together with ac...
Dissertation (Ph.D.) University of Alaska Fairbanks, 1995A comprehensive radiative transfer model fo...
The global climate is determined by the exchange of energy between the earth, atmosphere, and space....
International audienceThe Arctic atmosphere–surface system transmits visible light from the Sun to t...
Sea ice is a remarkable component of the global climate system. It can form over up to about 10 % of...
By means of simulations with a global coupled AOGCM it is shown that changes in the polar energy sin...
Determination of the energy fluxes resulting from incident solar radiation is fundamental to an unde...
The chapter describes meteorology in the polar regions, covering radiative transfer, atmospheric cir...
Summary: The partitioning of solar radiation in the Arctic sea ice during the melt season is investi...
Source code for the radiative transfer model (RAPRAD) used in the study Li et al. (2022)
For a considerable coverage the energy balance of and ice formation by leads in sea ice in the Wedde...
Abstract. A coupled global climate model is used to evaluate processes that determine the equilibriu...
The Arctic Ocean receives considerable input of terrigenous carbon supplied by the Arctic rivers. In...
The primary driver of the climate system is the uneven distribution of incoming and outgoing radiati...
Light (solar short-wave radiation) transmission into and through sea ice is of high importance for v...
The loss of Arctic sea ice has emerged as a leading signal of global warming. This, together with ac...
Dissertation (Ph.D.) University of Alaska Fairbanks, 1995A comprehensive radiative transfer model fo...
The global climate is determined by the exchange of energy between the earth, atmosphere, and space....
International audienceThe Arctic atmosphere–surface system transmits visible light from the Sun to t...
Sea ice is a remarkable component of the global climate system. It can form over up to about 10 % of...
By means of simulations with a global coupled AOGCM it is shown that changes in the polar energy sin...
Determination of the energy fluxes resulting from incident solar radiation is fundamental to an unde...
The chapter describes meteorology in the polar regions, covering radiative transfer, atmospheric cir...
Summary: The partitioning of solar radiation in the Arctic sea ice during the melt season is investi...
Source code for the radiative transfer model (RAPRAD) used in the study Li et al. (2022)
For a considerable coverage the energy balance of and ice formation by leads in sea ice in the Wedde...
Abstract. A coupled global climate model is used to evaluate processes that determine the equilibriu...
The Arctic Ocean receives considerable input of terrigenous carbon supplied by the Arctic rivers. In...
The primary driver of the climate system is the uneven distribution of incoming and outgoing radiati...
Light (solar short-wave radiation) transmission into and through sea ice is of high importance for v...
The loss of Arctic sea ice has emerged as a leading signal of global warming. This, together with ac...