A large-scale gravity wave (GW) was observed spanning the whole of Greenland. The GWs proposed in this paper come from a new jet-topography mechanism. The topography compresses the flow and triggers a change in u- and v-wind components. The jet becomes out of geostrophic balance and sheds energy in the form of GWs to restore the balance. This topography-jet interaction was not previously considered by the community, rendering the impact of the gravity waves largely unaccounted for
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
To better understand the impact of gravity waves (GWs) on the middle atmosphere in the current and f...
To better understand the impact of gravity waves (GWs) on the middle atmosphere in the current and f...
To better understand the impact of gravity waves (GWs) on the middle atmosphere in the current and f...
In order to improve global atmospheric modelling, the trend is towards including specific gravity wa...
In order to improve global atmospheric modelling, the trend is towards including source-specific gra...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
To better understand the impact of gravity waves (GWs) on the middle atmosphere in the current and f...
To better understand the impact of gravity waves (GWs) on the middle atmosphere in the current and f...
To better understand the impact of gravity waves (GWs) on the middle atmosphere in the current and f...
In order to improve global atmospheric modelling, the trend is towards including specific gravity wa...
In order to improve global atmospheric modelling, the trend is towards including source-specific gra...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...
International audienceA polar stratospheric ice cloud (PSC type II) was observed by airborne lidar a...