Add to ORKGA foehn wind is a warm, dry, downslope wind resulting from synoptic-scale, cross-barrier flow over a mountain range. Foehn winds are a climatologica
This study investigates the spatial structure and the seasonal occurrence of foehn wind to the east ...
Local scale windfield and air mass characteristics during the onset of two foehn wind events in an a...
Foehn winds in the lee of mountain barriers create highly favourable meteorological conditions for w...
Foehn winds resulting from topographic modification of airflow in the lee of mountain barriers are f...
Foehn winds are warm, dry and gusty downslope winds resulting from the topographic modification of t...
Foehn winds are a prominent feature of the McMurdo Dry Valleys (MDVs) climate, and are responsible f...
Foehn winds resulting from topographic modification of airflow in the lee of mountain barriers are f...
ABSTRACT: Warm, dry and gusty foehn winds are frequently experienced in the McMurdo Dry Valleys (MDV...
Foehn winds resulting from topographic modification of airflow in the lee of mountain barriers are f...
Warm, dry and gusty foehn winds are frequently experienced in the McMurdo Dry Valleys (MDVs), Antarc...
The foehn effect is well known as the warming, drying, and cloud clearance experienced on the lee si...
In the present study foehn clearance is described and compared with strong downslope windstorms like...
This study investigates the spatial structure and the seasonal occurrence of foehn wind to the east ...
The McMurdo Dry Valleys (MDV) are a polar desert, where glacial melt is the main source of water to ...
The McMurdo Dry Valleys (MDV) are a polar desert, where glacial melt is the main source of water to ...
This study investigates the spatial structure and the seasonal occurrence of foehn wind to the east ...
Local scale windfield and air mass characteristics during the onset of two foehn wind events in an a...
Foehn winds in the lee of mountain barriers create highly favourable meteorological conditions for w...
Foehn winds resulting from topographic modification of airflow in the lee of mountain barriers are f...
Foehn winds are warm, dry and gusty downslope winds resulting from the topographic modification of t...
Foehn winds are a prominent feature of the McMurdo Dry Valleys (MDVs) climate, and are responsible f...
Foehn winds resulting from topographic modification of airflow in the lee of mountain barriers are f...
ABSTRACT: Warm, dry and gusty foehn winds are frequently experienced in the McMurdo Dry Valleys (MDV...
Foehn winds resulting from topographic modification of airflow in the lee of mountain barriers are f...
Warm, dry and gusty foehn winds are frequently experienced in the McMurdo Dry Valleys (MDVs), Antarc...
The foehn effect is well known as the warming, drying, and cloud clearance experienced on the lee si...
In the present study foehn clearance is described and compared with strong downslope windstorms like...
This study investigates the spatial structure and the seasonal occurrence of foehn wind to the east ...
The McMurdo Dry Valleys (MDV) are a polar desert, where glacial melt is the main source of water to ...
The McMurdo Dry Valleys (MDV) are a polar desert, where glacial melt is the main source of water to ...
This study investigates the spatial structure and the seasonal occurrence of foehn wind to the east ...
Local scale windfield and air mass characteristics during the onset of two foehn wind events in an a...
Foehn winds in the lee of mountain barriers create highly favourable meteorological conditions for w...