The Real-Time Ultrafinescale Forecast Support during the Special Observing Period of the MAPSource: Bulletin of the American Meteorological Society:;2002:;volume( 083 ):;issue: 001::page 85Author:Benoit, R.
,
Schär, C.
,
Binder, P.
,
Chamberland, S.
,
Davies, H. C.
,
Desgagné, M.
,
Girard, C.
,
Keil, C.
,
Kouwen, N.
,
Lüthi, D.
,
Maric, D.
,
Müller, E.
,
Pellerin, P.
,
Schmidli, J.
,
Schubiger, F.
,
Schwierz, C.
,
Sprenger, M.
,
Walser, A.
,
Willemse, S.
,
Yu, W.
,
Zala, E.
DOI: 10.1175/1520-0477(2002)083<0085:TRTUFS>2.3.CO;2Publisher: American Meteorological Society
Abstract: Recent developments in numerical modeling and computer technology will soon allow for limited-areaproduction-type numerical weather prediction at a resolution of 1-2 km. This advance opens exciting prospects for the prediction of airflow and precipitation phenomena in and around mountainous regions, by improving the representation of the underlying topography, and by explicitly simulating (rather than parameterizing) moist convection. During the Special Observation Period (SOP; 7 Sept-15 Nov 1999) of the Mesoscale Alpine Programme (MAP) the Canadian Mesoscale Compressible Community Model (MC2) has been run in real time at a horizontal resolution of3 km on a computational domain of 350 ? 300 ? 50 grid points, covering the whole of the Alpine region. An overview of the model configuration and performance will be presented along with simulation and validation results fromselected MAP cases. Some critical aspects that require particular attention in future research will also be addressed.
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contributor author | Benoit, R. | |
contributor author | Schär, C. | |
contributor author | Binder, P. | |
contributor author | Chamberland, S. | |
contributor author | Davies, H. C. | |
contributor author | Desgagné, M. | |
contributor author | Girard, C. | |
contributor author | Keil, C. | |
contributor author | Kouwen, N. | |
contributor author | Lüthi, D. | |
contributor author | Maric, D. | |
contributor author | Müller, E. | |
contributor author | Pellerin, P. | |
contributor author | Schmidli, J. | |
contributor author | Schubiger, F. | |
contributor author | Schwierz, C. | |
contributor author | Sprenger, M. | |
contributor author | Walser, A. | |
contributor author | Willemse, S. | |
contributor author | Yu, W. | |
contributor author | Zala, E. | |
date accessioned | 2017-06-09T14:43:13Z | |
date available | 2017-06-09T14:43:13Z | |
date copyright | 2002/01/01 | |
date issued | 2002 | |
identifier issn | 0003-0007 | |
identifier other | ams-25178.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4161932 | |
description abstract | Recent developments in numerical modeling and computer technology will soon allow for limited-areaproduction-type numerical weather prediction at a resolution of 1-2 km. This advance opens exciting prospects for the prediction of airflow and precipitation phenomena in and around mountainous regions, by improving the representation of the underlying topography, and by explicitly simulating (rather than parameterizing) moist convection. During the Special Observation Period (SOP; 7 Sept-15 Nov 1999) of the Mesoscale Alpine Programme (MAP) the Canadian Mesoscale Compressible Community Model (MC2) has been run in real time at a horizontal resolution of3 km on a computational domain of 350 ? 300 ? 50 grid points, covering the whole of the Alpine region. An overview of the model configuration and performance will be presented along with simulation and validation results fromselected MAP cases. Some critical aspects that require particular attention in future research will also be addressed. | |
publisher | American Meteorological Society | |
title | The Real-Time Ultrafinescale Forecast Support during the Special Observing Period of the MAP | |
type | Journal Paper | |
journal volume | 83 | |
journal issue | 1 | |
journal title | Bulletin of the American Meteorological Society | |
identifier doi | 10.1175/1520-0477(2002)083<0085:TRTUFS>2.3.CO;2 | |
journal fristpage | 85 | |
journal lastpage | 109 | |
tree | Bulletin of the American Meteorological Society:;2002:;volume( 083 ):;issue: 001 | |
contenttype | Fulltext |