North-western Mediterranean sea-breeze circulation in a regional climate system model
In the Mediterranean basin, moisture transport can occur over large distance from remote regions by the synoptic circulation or more locally by sea breezes, driven by land-sea thermal contrast. Sea breezes play an important role in inland transport of moisture especially between late spring and earl...
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| Veröffentlicht in: | Climate dynamics 2018-08, Vol.51 (3), p.1077-1093 |
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| creator | Drobinski, Philippe Bastin, Sophie Arsouze, Thomas Béranger, Karine Flaounas, Emmanouil Stéfanon, Marc |
| description | In the Mediterranean basin, moisture transport can occur over large distance from remote regions by the synoptic circulation or more locally by sea breezes, driven by land-sea thermal contrast. Sea breezes play an important role in inland transport of moisture especially between late spring and early fall. In order to explicitly represent the two-way interactions at the atmosphere-ocean interface in the Mediterranean region and quantify the role of air-sea feedbacks on regional meteorology and climate, simulations at 20 km resolution performed with WRF regional climate model (RCM) and MORCE atmosphere-ocean regional climate model (AORCM) coupling WRF and NEMO-MED12 in the frame of HyMeX/MED-CORDEX are compared. One result of this study is that these simulations reproduce remarkably well the intensity, direction and inland penetration of the sea breeze and even the existence of the shallow sea breeze despite the overestimate of temperature over land in both simulations. The coupled simulation provides a more realistic representation of the evolution of the SST field at fine scale than the atmosphere-only one. Temperature and moisture anomalies are created in direct response to the SST anomaly and are advected by the sea breeze over land. However, the SST anomalies are not of sufficient magnitude to affect the large-scale sea-breeze circulation. The temperature anomalies are quickly damped by strong surface heating over land, whereas the water vapor mixing ratio anomalies are transported further inland. The inland limit of significance is imposed by the vertical dilution in a deeper continental boundary-layer. |
| doi_str_mv | 10.1007/s00382-017-3595-z |
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Sea breezes play an important role in inland transport of moisture especially between late spring and early fall. In order to explicitly represent the two-way interactions at the atmosphere-ocean interface in the Mediterranean region and quantify the role of air-sea feedbacks on regional meteorology and climate, simulations at 20 km resolution performed with WRF regional climate model (RCM) and MORCE atmosphere-ocean regional climate model (AORCM) coupling WRF and NEMO-MED12 in the frame of HyMeX/MED-CORDEX are compared. One result of this study is that these simulations reproduce remarkably well the intensity, direction and inland penetration of the sea breeze and even the existence of the shallow sea breeze despite the overestimate of temperature over land in both simulations. The coupled simulation provides a more realistic representation of the evolution of the SST field at fine scale than the atmosphere-only one. Temperature and moisture anomalies are created in direct response to the SST anomaly and are advected by the sea breeze over land. However, the SST anomalies are not of sufficient magnitude to affect the large-scale sea-breeze circulation. The temperature anomalies are quickly damped by strong surface heating over land, whereas the water vapor mixing ratio anomalies are transported further inland. The inland limit of significance is imposed by the vertical dilution in a deeper continental boundary-layer.</description><identifier>ISSN: 0930-7575</identifier><identifier>EISSN: 1432-0894</identifier><identifier>DOI: 10.1007/s00382-017-3595-z</identifier><language>eng</language><publisher>Berlin/Heidelberg: Springer Berlin Heidelberg</publisher><subject>Air circulation ; Anomalies ; Atmosphere ; Breeze circulation ; Breezes ; Climate ; Climate models ; Climate system ; Climatology ; Computer simulation ; Dilution ; Earth and Environmental Science ; Earth Sciences ; Evolution ; Geophysics/Geodesy ; Heating ; Interactions ; Meteorology ; Mixing ratio ; Moisture ; Ocean-atmosphere interaction ; Oceanography ; Oceans ; Ozone ; Regional climate models ; Regional climates ; Remote regions ; Sciences of the Universe ; Sea breezes ; Sea surface ; Simulation ; Surface temperature ; Temperature anomalies ; Temperature effects ; Transport ; Water vapor ; Water vapour</subject><ispartof>Climate dynamics, 2018-08, Vol.51 (3), p.1077-1093</ispartof><rights>The Author(s) 2017</rights><rights>COPYRIGHT 2018 Springer</rights><rights>Climate Dynamics is a copyright of Springer, (2017). 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Temperature and moisture anomalies are created in direct response to the SST anomaly and are advected by the sea breeze over land. However, the SST anomalies are not of sufficient magnitude to affect the large-scale sea-breeze circulation. The temperature anomalies are quickly damped by strong surface heating over land, whereas the water vapor mixing ratio anomalies are transported further inland. The inland limit of significance is imposed by the vertical dilution in a deeper continental boundary-layer.</description><subject>Air circulation</subject><subject>Anomalies</subject><subject>Atmosphere</subject><subject>Breeze circulation</subject><subject>Breezes</subject><subject>Climate</subject><subject>Climate models</subject><subject>Climate system</subject><subject>Climatology</subject><subject>Computer simulation</subject><subject>Dilution</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Evolution</subject><subject>Geophysics/Geodesy</subject><subject>Heating</subject><subject>Interactions</subject><subject>Meteorology</subject><subject>Mixing ratio</subject><subject>Moisture</subject><subject>Ocean-atmosphere interaction</subject><subject>Oceanography</subject><subject>Oceans</subject><subject>Ozone</subject><subject>Regional climate models</subject><subject>Regional climates</subject><subject>Remote 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Dyn</stitle><date>2018-08-01</date><risdate>2018</risdate><volume>51</volume><issue>3</issue><spage>1077</spage><epage>1093</epage><pages>1077-1093</pages><issn>0930-7575</issn><eissn>1432-0894</eissn><abstract>In the Mediterranean basin, moisture transport can occur over large distance from remote regions by the synoptic circulation or more locally by sea breezes, driven by land-sea thermal contrast. 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Temperature and moisture anomalies are created in direct response to the SST anomaly and are advected by the sea breeze over land. However, the SST anomalies are not of sufficient magnitude to affect the large-scale sea-breeze circulation. The temperature anomalies are quickly damped by strong surface heating over land, whereas the water vapor mixing ratio anomalies are transported further inland. The inland limit of significance is imposed by the vertical dilution in a deeper continental boundary-layer.</abstract><cop>Berlin/Heidelberg</cop><pub>Springer Berlin Heidelberg</pub><doi>10.1007/s00382-017-3595-z</doi><tpages>17</tpages><orcidid>https://orcid.org/0000-0001-9769-7817</orcidid><orcidid>https://orcid.org/0000-0002-8871-6120</orcidid><orcidid>https://orcid.org/0000-0003-1951-6798</orcidid><orcidid>https://orcid.org/0000-0002-8667-9899</orcidid><oa>free_for_read</oa></addata></record> |
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| subjects | Air circulation Anomalies Atmosphere Breeze circulation Breezes Climate Climate models Climate system Climatology Computer simulation Dilution Earth and Environmental Science Earth Sciences Evolution Geophysics/Geodesy Heating Interactions Meteorology Mixing ratio Moisture Ocean-atmosphere interaction Oceanography Oceans Ozone Regional climate models Regional climates Remote regions Sciences of the Universe Sea breezes Sea surface Simulation Surface temperature Temperature anomalies Temperature effects Transport Water vapor Water vapour |
| title | North-western Mediterranean sea-breeze circulation in a regional climate system model |
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