The results of measurements of net total radiation flux and temperatures in the air and surface layers of the tundra and snow near Barrow, Alaska, are presented for the period September 1965 to September 1966. Lowest average monthly temperatures occurred in March, the highest in July. The minimum average net total radiation occurred in January with the maximum in July. The tundra surface began to thaw by 18 June and to freeze by September.Processus physiques à la surface de la toundra arctique. Les auteurs présentent les résultats de mesures du flux de rayonnement total net et des températures dans l'air et dans les niveaux de surface de la toundra et de la neige, près de Barrow, Alaska, pour la pér...
In this study, we present the winter time surface energy balance at a polygonal tundra site in north...
Independent measurements of radiation, sensible and latent heat fluxes and the ground heat flux are ...
In this article, we present a study on the surface energy balance of a polygonal tundra landscape in...
The microclimate of the tundra during spring of 1971 (29 May to 17 June) at Barrow, is described and...
The effects of slope, aspect and vegetation cover on the radiation balance and active layer thermal ...
ABSTRACT. The vehicle-induced subsurface thaw response in a tussock tundra area was experimentally m...
Since 1959 the Geographical Branch of the Canada Department of Mines and Technical Surveys has been ...
Several climate change scenarios have predicted that the greatest changes would occur at high latitu...
This observational study compares seasonal variations of surface fluxes (turbulent, radiative, and s...
Meteorological observations on and around a small, exposed plateau ice cap on north-eastern Ellesmer...
The Arctic Boundary Layer Expedition (ABLE 3A) used measurements from ground, aircraft, and satellit...
International audienceThe structure of the snowpack near Barrow was studied in March-April 2009. Ver...
In this study, we present the winter time surface energy balance at a polygonal tundra site in north...
Passive warming manipulation methodologies, such as open-top chambers (OTCs), are a meaningful appro...
Observations led to a study of the physical properties of snow and the processes which operate on it...
In this study, we present the winter time surface energy balance at a polygonal tundra site in north...
Independent measurements of radiation, sensible and latent heat fluxes and the ground heat flux are ...
In this article, we present a study on the surface energy balance of a polygonal tundra landscape in...
The microclimate of the tundra during spring of 1971 (29 May to 17 June) at Barrow, is described and...
The effects of slope, aspect and vegetation cover on the radiation balance and active layer thermal ...
ABSTRACT. The vehicle-induced subsurface thaw response in a tussock tundra area was experimentally m...
Since 1959 the Geographical Branch of the Canada Department of Mines and Technical Surveys has been ...
Several climate change scenarios have predicted that the greatest changes would occur at high latitu...
This observational study compares seasonal variations of surface fluxes (turbulent, radiative, and s...
Meteorological observations on and around a small, exposed plateau ice cap on north-eastern Ellesmer...
The Arctic Boundary Layer Expedition (ABLE 3A) used measurements from ground, aircraft, and satellit...
International audienceThe structure of the snowpack near Barrow was studied in March-April 2009. Ver...
In this study, we present the winter time surface energy balance at a polygonal tundra site in north...
Passive warming manipulation methodologies, such as open-top chambers (OTCs), are a meaningful appro...
Observations led to a study of the physical properties of snow and the processes which operate on it...
In this study, we present the winter time surface energy balance at a polygonal tundra site in north...
Independent measurements of radiation, sensible and latent heat fluxes and the ground heat flux are ...
In this article, we present a study on the surface energy balance of a polygonal tundra landscape in...