The present report povides technical background information to the study of Egerer et al. (2023) on the role of a low-level jet (LLJ) for stirring the stable atmospheric surface layer in the Arctic. Based on micrometeorological tower measurements and tethered balloon-borne hot-wire anemometer measurements conducted during a 15 h observation period during the PAMARCMiP field experiment at the Villum Research Station (VRS, Station Nord) in North-East Greenland (March 28-30, 2018). Egerer et al. (2023) analyzed the transition of a stable atmospheric boundary layer (ABL) with a LLJ into a traditional stable ABL in the late-winter central Arctic
International audienceObservations from CMET (Controlled Meteorological) balloons are analysed to pr...
International audienceObservations from CMET (Controlled Meteorological) balloons are analysed to pr...
We analyze the Northern Hemisphere atmospheric response to Arctic sea ice decline in the CNRM-CM6 mo...
We present an annual characterization of low-level jets (LLJs) over the Arctic Ocean using wind prof...
We present an annual characterization of low-level jets (LLJs) over the Arctic Ocean using wind prof...
Clouds play an important role in Arctic amplification. This term represents the recently observed en...
Low-level atmospheric jets have been observed to occur frequently in marginal ice zones (MIZs), but ...
A consortium of polar scientists combined observational forces in a field campaign of unprecedented ...
The fact that severe weather associated with polar lows and arctic fronts still comes unforeseen and...
The article of record as published may be found at https://doi.org/10.1002/2018JC013778During the Se...
International audienceObservations from CMET (Controlled Meteorological) balloons are analyzed in co...
International audienceObservations from CMET (Controlled Meteorological) balloons are analyzed in co...
International audienceObservations from CMET (Controlled Meteorological) balloons are analyzed in co...
L’étude de l’atmosphère arctique présente un intérêt scientifique grandissant, la température de sa ...
Aerosol particles are considered to be one of the main contributors in affecting the feedback mechan...
International audienceObservations from CMET (Controlled Meteorological) balloons are analysed to pr...
International audienceObservations from CMET (Controlled Meteorological) balloons are analysed to pr...
We analyze the Northern Hemisphere atmospheric response to Arctic sea ice decline in the CNRM-CM6 mo...
We present an annual characterization of low-level jets (LLJs) over the Arctic Ocean using wind prof...
We present an annual characterization of low-level jets (LLJs) over the Arctic Ocean using wind prof...
Clouds play an important role in Arctic amplification. This term represents the recently observed en...
Low-level atmospheric jets have been observed to occur frequently in marginal ice zones (MIZs), but ...
A consortium of polar scientists combined observational forces in a field campaign of unprecedented ...
The fact that severe weather associated with polar lows and arctic fronts still comes unforeseen and...
The article of record as published may be found at https://doi.org/10.1002/2018JC013778During the Se...
International audienceObservations from CMET (Controlled Meteorological) balloons are analyzed in co...
International audienceObservations from CMET (Controlled Meteorological) balloons are analyzed in co...
International audienceObservations from CMET (Controlled Meteorological) balloons are analyzed in co...
L’étude de l’atmosphère arctique présente un intérêt scientifique grandissant, la température de sa ...
Aerosol particles are considered to be one of the main contributors in affecting the feedback mechan...
International audienceObservations from CMET (Controlled Meteorological) balloons are analysed to pr...
International audienceObservations from CMET (Controlled Meteorological) balloons are analysed to pr...
We analyze the Northern Hemisphere atmospheric response to Arctic sea ice decline in the CNRM-CM6 mo...