Mediterranean contemporary winter and summer air mass climatology with respect to temperature and moisture flux

Large-scale moisture fluxes and backward air mass trajectories and frequencies were investigated to explain the mechanisms of synoptic-scale seasonal variability of air masses in the Mediterranean basin. For this aim, reanalysis data were used to calculate variations in moisture flux with respect to...

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Published in:Climate Research
Main Author: Şahin, Serdar
Format: Article in Journal/Newspaper
Language:English
Published: Inter-Research 2021
Subjects:
Online Access:https://hdl.handle.net/20.500.11776/11153
https://doi.org/10.3354/cr01664
id ftnamikkemaluniv:oai:acikerisim.nku.edu.tr:20.500.11776/11153
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spelling ftnamikkemaluniv:oai:acikerisim.nku.edu.tr:20.500.11776/11153 2023-10-01T03:54:01+02:00 Mediterranean contemporary winter and summer air mass climatology with respect to temperature and moisture flux Şahin, Serdar 2021 https://hdl.handle.net/20.500.11776/11153 https://doi.org/10.3354/cr01664 eng eng Inter-Research Climate Research Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı 0936-577X https://doi.org/10.3354/cr01664 https://hdl.handle.net/20.500.11776/11153 doi:10.3354/cr01664 84 159 179 2-s2.0-85128661421 info:eu-repo/semantics/closedAccess Air mass Frequency Mediterranean basin Moisture flux Trajectory air temperature climatology Mediterranean environment summer surface pressure winter Arctic Atlantic Ocean Mediterranean Sea article 2021 ftnamikkemaluniv https://doi.org/20.500.11776/1115310.3354/cr01664 2023-09-03T19:17:55Z Large-scale moisture fluxes and backward air mass trajectories and frequencies were investigated to explain the mechanisms of synoptic-scale seasonal variability of air masses in the Mediterranean basin. For this aim, reanalysis data were used to calculate variations in moisture flux with respect to temperature and stability according to the 8 standard pressure levels between 1000 and 300 hPa. Investigating air mass characteristics changing with pressure levels provided new information in terms of air mass climatology for the Mediterranean basin. Results show that due to the influence of westerly flows, the Atlantic is the main source of moisture higher than 700 hPa. Turbulent transport of moisture from the Mediterranean Sea is the source of moisture close to the surface, which corresponds to levels lower than 700 hPa. According to the trajectory analysis, the continental Arctic (cA) air mass can reach the Mediterranean basin and provide very wet conditions over the Mediterranean basin during winter. In addition, during very dry conditions in summer, all air mass currents originate from surface pressure levels between 1000 and 850 hPa. These relatively warm and dominant air masses cause cloud-free conditions with very low precipitation over the Mediterranean basin. This study showed that air masses should be analyzed not only according to their source and path but also according to pressure levels. Therefore, more studies are needed investigating the contemporary air mass climatology of a specific region. © Inter-Research 2021 National Oceanic and Atmospheric Administration, NOAA; National Center for Atmospheric Research, NCAR; University Corporation for Atmospheric Research, UCAR; Office of AIDS Research, OAR; Earth System Research Laboratories, ESRL; Computational and Information Systems Laboratory, CISL I thank Prof. Dr. Murat Türkeş for his valuable publications, ideas and comments that inspired me to this work. Also, I thank 3 anonymous reviewers and the in-house editors for their valuable comments on ... Article in Journal/Newspaper Arctic Namık Kemal University Institutional Repository Arctic Climate Research 84 159 179
institution Open Polar
collection Namık Kemal University Institutional Repository
op_collection_id ftnamikkemaluniv
language English
topic Air mass
Frequency
Mediterranean basin
Moisture flux
Trajectory
air temperature
climatology
Mediterranean environment
summer
surface pressure
winter
Arctic
Atlantic Ocean
Mediterranean Sea
spellingShingle Air mass
Frequency
Mediterranean basin
Moisture flux
Trajectory
air temperature
climatology
Mediterranean environment
summer
surface pressure
winter
Arctic
Atlantic Ocean
Mediterranean Sea
Şahin, Serdar
Mediterranean contemporary winter and summer air mass climatology with respect to temperature and moisture flux
topic_facet Air mass
Frequency
Mediterranean basin
Moisture flux
Trajectory
air temperature
climatology
Mediterranean environment
summer
surface pressure
winter
Arctic
Atlantic Ocean
Mediterranean Sea
description Large-scale moisture fluxes and backward air mass trajectories and frequencies were investigated to explain the mechanisms of synoptic-scale seasonal variability of air masses in the Mediterranean basin. For this aim, reanalysis data were used to calculate variations in moisture flux with respect to temperature and stability according to the 8 standard pressure levels between 1000 and 300 hPa. Investigating air mass characteristics changing with pressure levels provided new information in terms of air mass climatology for the Mediterranean basin. Results show that due to the influence of westerly flows, the Atlantic is the main source of moisture higher than 700 hPa. Turbulent transport of moisture from the Mediterranean Sea is the source of moisture close to the surface, which corresponds to levels lower than 700 hPa. According to the trajectory analysis, the continental Arctic (cA) air mass can reach the Mediterranean basin and provide very wet conditions over the Mediterranean basin during winter. In addition, during very dry conditions in summer, all air mass currents originate from surface pressure levels between 1000 and 850 hPa. These relatively warm and dominant air masses cause cloud-free conditions with very low precipitation over the Mediterranean basin. This study showed that air masses should be analyzed not only according to their source and path but also according to pressure levels. Therefore, more studies are needed investigating the contemporary air mass climatology of a specific region. © Inter-Research 2021 National Oceanic and Atmospheric Administration, NOAA; National Center for Atmospheric Research, NCAR; University Corporation for Atmospheric Research, UCAR; Office of AIDS Research, OAR; Earth System Research Laboratories, ESRL; Computational and Information Systems Laboratory, CISL I thank Prof. Dr. Murat Türkeş for his valuable publications, ideas and comments that inspired me to this work. Also, I thank 3 anonymous reviewers and the in-house editors for their valuable comments on ...
format Article in Journal/Newspaper
author Şahin, Serdar
author_facet Şahin, Serdar
author_sort Şahin, Serdar
title Mediterranean contemporary winter and summer air mass climatology with respect to temperature and moisture flux
title_short Mediterranean contemporary winter and summer air mass climatology with respect to temperature and moisture flux
title_full Mediterranean contemporary winter and summer air mass climatology with respect to temperature and moisture flux
title_fullStr Mediterranean contemporary winter and summer air mass climatology with respect to temperature and moisture flux
title_full_unstemmed Mediterranean contemporary winter and summer air mass climatology with respect to temperature and moisture flux
title_sort mediterranean contemporary winter and summer air mass climatology with respect to temperature and moisture flux
publisher Inter-Research
publishDate 2021
url https://hdl.handle.net/20.500.11776/11153
https://doi.org/10.3354/cr01664
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_relation Climate Research
Makale - Uluslararası Hakemli Dergi - Kurum Öğretim Elemanı
0936-577X
https://doi.org/10.3354/cr01664
https://hdl.handle.net/20.500.11776/11153
doi:10.3354/cr01664
84
159
179
2-s2.0-85128661421
op_rights info:eu-repo/semantics/closedAccess
op_doi https://doi.org/20.500.11776/1115310.3354/cr01664
container_title Climate Research
container_volume 84
container_start_page 159
op_container_end_page 179
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