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Partitioning of Snowy and Rainy Precipitation in a Case of a North Adriatic Frontal Passage : Volume 7, Issue 7 (18/04/2006)

By Monai, M.

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Book Id: WPLBN0003972681
Format Type: PDF Article :
File Size: Pages 6
Reproduction Date: 2015

Title: Partitioning of Snowy and Rainy Precipitation in a Case of a North Adriatic Frontal Passage : Volume 7, Issue 7 (18/04/2006)  
Author: Monai, M.
Volume: Vol. 7, Issue 7
Language: English
Subject: Science, Advances, Geosciences
Collections: Periodicals: Journal and Magazine Collection, Copernicus GmbH
Historic
Publication Date:
2006
Publisher: Copernicus Gmbh, Göttingen, Germany
Member Page: Copernicus Publications

Citation

APA MLA Chicago

Bonan, A. C., Rossa, A. M., & Monai, M. (2006). Partitioning of Snowy and Rainy Precipitation in a Case of a North Adriatic Frontal Passage : Volume 7, Issue 7 (18/04/2006). Retrieved from http://www.ebooklibrary.org/


Description
Description: Meteorological Center of Teolo, ARPA Veneto, Italy. A case of snow fall in the plains of the Northern Italian region Veneto is presented from a forecasters' perspective. Contrasting forecast guidance came from the ECMWF global model and the limited area model LAMI. The former showed a marked warm-moist Sirocco flow coming from the Adriatic Sea onto the coast at all levels, the latter discerned a distinct cold air flow from the north-east along the foothills of the Alps. The integrated observing network of the Centro Meteorologico di Teolo ARPA Veneto revealed this cold-air structure and helped the forecaster in the choice of the forecast and underpin the snowfall alert to the road authorities. It is argued that this feature is a crucial element for the occurrence of snowfall over the Veneto plains, and that the high-resolution numerical weather prediction model was essential in describing this mesoscale feature. The nature of the north-easterly flow is thought to be a combination of a Bora like flow and a barrier jet induced by flow blocking by the Alps.

Summary
Partitioning of snowy and rainy precipitation in a case of a north Adriatic frontal passage

 

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