The different methods of the numerical analysis of the small-scale features observed during MAP IOP cases are compared. The products from the MAP ECMWF Re-analysis are compared with the other analysis products. The properties of downscaling of MAP ECMWF Re-analysis to the meso-beta resolution are examined. The “blending initialisation method” developed under the ALADIN Project is applied as the initialisation technique. MAP IOP2 case has declared as the most intensive and complex event during MAP IOP period. The strong south flow intrusion into the Rhone valley on 20 September 1999 at 00 UTC has been measured by Lyon radiosonde. The tests describe how the analysis of low-level jet has been improved by the “blending initialisation method”
An extensive analysis of Low Level Jets (LLJs) over the Southern North Sea is presented. The study i...
This study explores simulations using the numerical Weather Research and Forecasting (WRF) model, wi...
Numerical simulations of the convective system observed during the MAP IOP2a have been performed wit...
A low-level jet (LLJ) event observed during a frontal passage in the 2001 Coupled Boundary Layers an...
International audienceA case study of a low-level jet (LLJ) during the OPALE (Oxidant Production ove...
A low-level jet (LLJ) event observed during a frontal passage in the 2001 Coupled Boundary Layers an...
Numerical simulations of the precipitation system during the MAP IOP5 and the extreme Bura wind case...
In order to better understand the influence of initial and boundary conditions on the numerical mode...
Due to the character of the original source materials and the nature of batch digitization, quality ...
Two cases of low-level jet (LLJ) support the hypothesis that the LLJ is an integral part of synoptic...
The atmosphere is a complex system with an infinite number of independent variables. The best approx...
International audienceThe HYDROPTIMET case studies (9?10 June 2000 Catalogne, 8?9 September 2002 Cév...
The classic Great Plains southerly low-level jet (LLJ) is a primary factor in sustaining nocturnal c...
During Intensive Observing Periods (IOP) of the Mesoscale Alpine Programme (MAP, see Bougeault et a...
This paper investigates the fundamental processes involved in a severe Mistral event that occurred d...
An extensive analysis of Low Level Jets (LLJs) over the Southern North Sea is presented. The study i...
This study explores simulations using the numerical Weather Research and Forecasting (WRF) model, wi...
Numerical simulations of the convective system observed during the MAP IOP2a have been performed wit...
A low-level jet (LLJ) event observed during a frontal passage in the 2001 Coupled Boundary Layers an...
International audienceA case study of a low-level jet (LLJ) during the OPALE (Oxidant Production ove...
A low-level jet (LLJ) event observed during a frontal passage in the 2001 Coupled Boundary Layers an...
Numerical simulations of the precipitation system during the MAP IOP5 and the extreme Bura wind case...
In order to better understand the influence of initial and boundary conditions on the numerical mode...
Due to the character of the original source materials and the nature of batch digitization, quality ...
Two cases of low-level jet (LLJ) support the hypothesis that the LLJ is an integral part of synoptic...
The atmosphere is a complex system with an infinite number of independent variables. The best approx...
International audienceThe HYDROPTIMET case studies (9?10 June 2000 Catalogne, 8?9 September 2002 Cév...
The classic Great Plains southerly low-level jet (LLJ) is a primary factor in sustaining nocturnal c...
During Intensive Observing Periods (IOP) of the Mesoscale Alpine Programme (MAP, see Bougeault et a...
This paper investigates the fundamental processes involved in a severe Mistral event that occurred d...
An extensive analysis of Low Level Jets (LLJs) over the Southern North Sea is presented. The study i...
This study explores simulations using the numerical Weather Research and Forecasting (WRF) model, wi...
Numerical simulations of the convective system observed during the MAP IOP2a have been performed wit...