International audienceA case study of a low-level jet (LLJ) during the OPALE (Oxidant Production over Antarctic Land and its Export) summer campaign is presented. It has been observed at Dome C (East Antarctica) and is simulated accurately by the three-dimensional version of the Modèle Atmosphérique Régional (MAR). It is found that this low-level jet is not related to an episode of thermal wind, suggesting that Dome C may be a place where turbulence on flat terrain can be studied
The regional climate model MAR was run for the region of Dome C located on the East Antarctic platea...
Mesoscale model simulations are presented of a westerly föhn event over the Antarctic Peninsula moun...
Low-level jets (LLJ) occur in many regions around the world and exhibit a diverse range of impacts a...
International audienceA case study of a low-level jet (LLJ) during the OPALE (Oxidant Production ove...
Two cases of low-level jet (LLJ) support the hypothesis that the LLJ is an integral part of synoptic...
International audienceThe ice-sheet offers us ”laboratory cases” with endless snow covered, relative...
Low-level jets (LLJs) are climatological features in polar regions. It is well known that katabatic ...
A unique dataset obtained with combinations of minisodars and 915-MHz wind profilers at the Atmosphe...
Low-level-jet (LLJ) periods are investigated by exploiting a long-termrecord of ground-based remote ...
Low-level atmospheric jets have been observed to occur frequently in marginal ice zones (MIZs), but ...
An extensive analysis of Low Level Jets (LLJs) over the Southern North Sea is presented. The study i...
We present the first observational evidence for convectively generated cold pools (CP) as driving me...
A review of 15 cases of low level jets (LLJ) which developed in the Great Plains is presented. For 1...
We present an annual characterization of low-level jets (LLJs) over the Arctic Ocean using wind prof...
© Copyright 1998 American Meteorological Society (AMS). Permission to use figures, tables, and brief...
The regional climate model MAR was run for the region of Dome C located on the East Antarctic platea...
Mesoscale model simulations are presented of a westerly föhn event over the Antarctic Peninsula moun...
Low-level jets (LLJ) occur in many regions around the world and exhibit a diverse range of impacts a...
International audienceA case study of a low-level jet (LLJ) during the OPALE (Oxidant Production ove...
Two cases of low-level jet (LLJ) support the hypothesis that the LLJ is an integral part of synoptic...
International audienceThe ice-sheet offers us ”laboratory cases” with endless snow covered, relative...
Low-level jets (LLJs) are climatological features in polar regions. It is well known that katabatic ...
A unique dataset obtained with combinations of minisodars and 915-MHz wind profilers at the Atmosphe...
Low-level-jet (LLJ) periods are investigated by exploiting a long-termrecord of ground-based remote ...
Low-level atmospheric jets have been observed to occur frequently in marginal ice zones (MIZs), but ...
An extensive analysis of Low Level Jets (LLJs) over the Southern North Sea is presented. The study i...
We present the first observational evidence for convectively generated cold pools (CP) as driving me...
A review of 15 cases of low level jets (LLJ) which developed in the Great Plains is presented. For 1...
We present an annual characterization of low-level jets (LLJs) over the Arctic Ocean using wind prof...
© Copyright 1998 American Meteorological Society (AMS). Permission to use figures, tables, and brief...
The regional climate model MAR was run for the region of Dome C located on the East Antarctic platea...
Mesoscale model simulations are presented of a westerly föhn event over the Antarctic Peninsula moun...
Low-level jets (LLJ) occur in many regions around the world and exhibit a diverse range of impacts a...
DOI
Add to ORKG