Abstract. The Tibetan Plateau (TP) has long been identified to be critical in regulating the Asian monsoon climate and hydrological cycle. In this modeling study a series of numer-ical experiments with a global climate model are designed to simulate radiative effect of black carbon (BC) and dust in snow, and to assess the relative impacts of anthropogenic CO2 and carbonaceous particles in the atmosphere and snow on the snowpack over the TP and subsequent impacts on the Asian monsoon climate and hydrological cycle. Simulations results show a large BC content in snow over the TP, espe-cially the southern slope. Because of the high aerosol content in snow and large incident solar radiation in the low latitude and high elevation, the TP exhibit...
Abstract. The remote and high elevation regions of central Asia are influenced by black carbon (BC) ...
Himalayan mountain glaciers and the snowpack over the Tibetan Plateau provide the headwater of seve...
Black carbon (BC) particles over the Himalayas and Tibetan Plateau (HTP), both airborne and those de...
A regional climate model (RegCM4.3.4) coupled with an aerosol–snow/ice feedback module was used to s...
Black carbon (BC), also known as soot, has been identified as the second most important anthropogeni...
The Tibetan Plateau (TP) has long been identified to be critical in regulating the Asian monsoon cli...
Snow cover plays a key role for sustaining ecology and society in mountainous regions. Light-absorbi...
Abstract We estimate the snow albedo forcing and direct radiative forcing (DRF) of black carbon (BC)...
International audienceWe applied a climate-chemistry global model to evaluate the impact of black ca...
The black carbon (BC) deposition on the ice core at Muztagh Ata Mountain, northern Tibetan Plateau, ...
The Tibetan Plateau (TP) plays important roles in global climate and environment. This study combine...
We quantified the impacts of variations in meteorological parameters and emissions on decadal, inter...
In the Tibetan Plateau, the black carbon (BC) concentration in surface snow and snow pits has receiv...
Abstract. The remote and high elevation regions of central Asia are influenced by black carbon (BC) ...
Himalayan mountain glaciers and the snowpack over the Tibetan Plateau provide the headwater of seve...
Black carbon (BC) particles over the Himalayas and Tibetan Plateau (HTP), both airborne and those de...
A regional climate model (RegCM4.3.4) coupled with an aerosol–snow/ice feedback module was used to s...
Black carbon (BC), also known as soot, has been identified as the second most important anthropogeni...
The Tibetan Plateau (TP) has long been identified to be critical in regulating the Asian monsoon cli...
Snow cover plays a key role for sustaining ecology and society in mountainous regions. Light-absorbi...
Abstract We estimate the snow albedo forcing and direct radiative forcing (DRF) of black carbon (BC)...
International audienceWe applied a climate-chemistry global model to evaluate the impact of black ca...
The black carbon (BC) deposition on the ice core at Muztagh Ata Mountain, northern Tibetan Plateau, ...
The Tibetan Plateau (TP) plays important roles in global climate and environment. This study combine...
We quantified the impacts of variations in meteorological parameters and emissions on decadal, inter...
In the Tibetan Plateau, the black carbon (BC) concentration in surface snow and snow pits has receiv...
Abstract. The remote and high elevation regions of central Asia are influenced by black carbon (BC) ...
Himalayan mountain glaciers and the snowpack over the Tibetan Plateau provide the headwater of seve...
Black carbon (BC) particles over the Himalayas and Tibetan Plateau (HTP), both airborne and those de...