Evaluation of the moisture sources in two extreme landfalling atmospheric river events using an Eulerian WRF tracers tool

A new 3-D tracer tool is coupled to the WRF model to analyze the origin of the moisture in two extreme atmospheric river (AR) events: the so-called Great Coastal Gale of 2007 in the Pacific Ocean and the Great Storm of 1987 in the North Atlantic. Results show that between 80 and 90 % of moisture adv...

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Published inEarth system dynamics Vol. 8; no. 4; pp. 1247 - 1261
Main Authors Eiras-Barca, Jorge, Dominguez, Francina, Hu, Huancui, Garaboa-Paz, Daniel, Miguez-Macho, Gonzalo
Format Journal Article
LanguageEnglish
Published Gottingen Copernicus GmbH 22.12.2017
Copernicus Publications
Subjects
Coasts
Cold
Cold front
Cold fronts
Cyclones
Evaluation
Extratropical cyclones
Fatalities
Floods
Humidity
Losses
Low-level jets
Measurement
Moisture
Moisture content
Precipitation
Rainfall
Rainfall reliability
Storms
Tracers
Tropical climate
Tropical climates
Typhoons
Water content
Weather
Iberian Peninsula
United States > US
British Isles
Europe
Atlantic Ocean
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Abstract A new 3-D tracer tool is coupled to the WRF model to analyze the origin of the moisture in two extreme atmospheric river (AR) events: the so-called Great Coastal Gale of 2007 in the Pacific Ocean and the Great Storm of 1987 in the North Atlantic. Results show that between 80 and 90 % of moisture advected by the ARs, and a high percentage of the total precipitation produced by the systems have a tropical origin. The tropical contribution to precipitation is in general above 50 % and largely exceeds this value in the most affected areas. Local convergence transport is responsible for the remaining moisture and precipitation. The ratio of tropical moisture to total moisture is maximized as the cold front arrives on land. Vertical cross sections of the moisture content suggest that the maximum in tropical humidity does not necessarily coincide with the low-level jet (LLJ) of the extratropical cyclone. Instead, the amount of tropical humidity is maximized in the lowest atmospheric level in southern latitudes and can be located above, below or ahead of the LLJ in northern latitudes in both analyzed cases.
AbstractList A new 3-D tracer tool is coupled to the WRF model to analyze the origin of the moisture in two extreme atmospheric river (AR) events: the so-called Great Coastal Gale of 2007 in the Pacific Ocean and the Great Storm of 1987 in the North Atlantic. Results show that between 80 and 90 % of moisture advected by the ARs, and a high percentage of the total precipitation produced by the systems have a tropical origin. The tropical contribution to precipitation is in general above 50 % and largely exceeds this value in the most affected areas. Local convergence transport is responsible for the remaining moisture and precipitation. The ratio of tropical moisture to total moisture is maximized as the cold front arrives on land. Vertical cross sections of the moisture content suggest that the maximum in tropical humidity does not necessarily coincide with the low-level jet (LLJ) of the extratropical cyclone. Instead, the amount of tropical humidity is maximized in the lowest atmospheric level in southern latitudes and can be located above, below or ahead of the LLJ in northern latitudes in both analyzed cases.
Audience Academic
Author Garaboa-Paz, Daniel
Hu, Huancui
Dominguez, Francina
Miguez-Macho, Gonzalo
Eiras-Barca, Jorge
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Snippet A new 3-D tracer tool is coupled to the WRF model to analyze the origin of the moisture in two extreme atmospheric river (AR) events: the so-called Great...
A new 3-D tracer tool is coupled to the WRF model to analyze the origin of the moisture in two extreme atmospheric river (AR) events: the so-called “Great...
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SubjectTerms Coasts
Cold
Cold front
Cold fronts
Cyclones
Evaluation
Extratropical cyclones
Fatalities
Floods
Humidity
Losses
Low-level jets
Measurement
Moisture
Moisture content
Precipitation
Rainfall
Rainfall reliability
Storms
Tracers
Tropical climate
Tropical climates
Typhoons
Water content
Weather
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Title Evaluation of the moisture sources in two extreme landfalling atmospheric river events using an Eulerian WRF tracers tool
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