Add to ORKGThe Tenth Symposium on Polar Science/Ordinary sessions: [OM] Polar Meteorology and Glaciology, Thu. 5 Dec. / 2F Auditorium , National Institute of Polar Researc
Short-lived aerosols such as black carbon (BC) and dust are important components of climate forcing,...
Black carbon (BC) is an aerosol material produced by incomplete combustion of fossil fuels and bioma...
Modeling studies show that the darkening of snow and ice by black carbon deposition is a major facto...
The Ninth Symposium on Polar Science/Ordinary sessions: [OM] Polar meteorology and glaciology, Wed. ...
The Ninth Symposium on Polar Science/Ordinary sessions: [OM] Polar meteorology and glaciology, Wed. ...
Key Points: • First ever measurements with a high‐accuracy single‐particle soot photometer of bla...
The 11th Symposium on Polar Science/Special session: [S] Accelerating Arctic research: Recent progre...
Long-term monitoring of atmospheric aerosols and their interaction with radiation, cloud, and cryosp...
Light absorbing aerosols (LAAs), such as black carbon (BC), in snow and ice are one of the least und...
Mass concentrations of aerosol black carbon (BC) and of the composite (total) aerosols (MB and MT, r...
An extended‐range Single Particle Soot Photometer (SP2) coupled to a Marin‐5 nebulizer was used to m...
Black carbon (BC) is a significant forcing agent in the Arctic, but substantial uncertainty remains ...
Black carbon (BC) particles in snow can significantly reduce the snow albedo and enhance the absorpt...
第8回極域科学シンポジウム/横断セッション：[IA] 北極国際連携拠点の新展開12月8日（金）国立極地研究所 2階大会議室The Eighth Symposium on Polar Science/I...
The distribution of black carbon (BC) in the atmosphere and the deposition of BC on snow surfaces si...
Short-lived aerosols such as black carbon (BC) and dust are important components of climate forcing,...
Black carbon (BC) is an aerosol material produced by incomplete combustion of fossil fuels and bioma...
Modeling studies show that the darkening of snow and ice by black carbon deposition is a major facto...
The Ninth Symposium on Polar Science/Ordinary sessions: [OM] Polar meteorology and glaciology, Wed. ...
The Ninth Symposium on Polar Science/Ordinary sessions: [OM] Polar meteorology and glaciology, Wed. ...
Key Points: • First ever measurements with a high‐accuracy single‐particle soot photometer of bla...
The 11th Symposium on Polar Science/Special session: [S] Accelerating Arctic research: Recent progre...
Long-term monitoring of atmospheric aerosols and their interaction with radiation, cloud, and cryosp...
Light absorbing aerosols (LAAs), such as black carbon (BC), in snow and ice are one of the least und...
Mass concentrations of aerosol black carbon (BC) and of the composite (total) aerosols (MB and MT, r...
An extended‐range Single Particle Soot Photometer (SP2) coupled to a Marin‐5 nebulizer was used to m...
Black carbon (BC) is a significant forcing agent in the Arctic, but substantial uncertainty remains ...
Black carbon (BC) particles in snow can significantly reduce the snow albedo and enhance the absorpt...
第8回極域科学シンポジウム/横断セッション：[IA] 北極国際連携拠点の新展開12月8日（金）国立極地研究所 2階大会議室The Eighth Symposium on Polar Science/I...
The distribution of black carbon (BC) in the atmosphere and the deposition of BC on snow surfaces si...
Short-lived aerosols such as black carbon (BC) and dust are important components of climate forcing,...
Black carbon (BC) is an aerosol material produced by incomplete combustion of fossil fuels and bioma...
Modeling studies show that the darkening of snow and ice by black carbon deposition is a major facto...