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The influence of atmospheric circulation types on regional patterns of precipitation in Marmara (NW Turkey)
In this study, regional patterns of precipitation in Marmara are described for the first time by means of Ward’s hierarchical cluster analysis. Daily values of winter precipitation data based on 19 meteorological stations were used for the period from 1960 to 2012. Five clusters of coherent zones we...
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Published in: | Theoretical and applied climatology 2017-02, Vol.127 (3-4), p.563-572 |
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description | In this study, regional patterns of precipitation in Marmara are described for the first time by means of Ward’s hierarchical cluster analysis. Daily values of winter precipitation data based on 19 meteorological stations were used for the period from 1960 to 2012. Five clusters of coherent zones were determined, namely Black Sea-Marmara, Black Sea, Marmara, Thrace, and Aegean sub-regions. To investigate the prevailing atmospheric circulation types (CTs) that cause precipitation occurrence and intensity in these five different rainfall sub-basins, objective Lamb weather type (LWT) methodology was applied to National Centers of Environmental Prediction (NCEP)/National Center for Atmospheric Research (NCAR) reanalysis of daily mean sea level pressure (MSLP) data. Precipitation occurrence suggested that wet CTs (i.e. N, NE, NW, and C) offer a high chance of precipitation in all sub-regions. For the eastern (western) part of the region, the high probability of rainfall occurrence is shown under the influence of E (SE, S, SW) atmospheric CTs. In terms of precipitation intensity, N and C CTs had the highest positive gradients in all the sub-basins of the Marmara. In addition, although Marmara and Black Sea sub-regions have the highest daily rainfall potential during NE types, high daily rainfall totals are recorded in all sub-regions except the Black Sea during NW types. |
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Daily values of winter precipitation data based on 19 meteorological stations were used for the period from 1960 to 2012. Five clusters of coherent zones were determined, namely Black Sea-Marmara, Black Sea, Marmara, Thrace, and Aegean sub-regions. To investigate the prevailing atmospheric circulation types (CTs) that cause precipitation occurrence and intensity in these five different rainfall sub-basins, objective Lamb weather type (LWT) methodology was applied to National Centers of Environmental Prediction (NCEP)/National Center for Atmospheric Research (NCAR) reanalysis of daily mean sea level pressure (MSLP) data. Precipitation occurrence suggested that wet CTs (i.e. N, NE, NW, and C) offer a high chance of precipitation in all sub-regions. For the eastern (western) part of the region, the high probability of rainfall occurrence is shown under the influence of E (SE, S, SW) atmospheric CTs. In terms of precipitation intensity, N and C CTs had the highest positive gradients in all the sub-basins of the Marmara. 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Daily values of winter precipitation data based on 19 meteorological stations were used for the period from 1960 to 2012. Five clusters of coherent zones were determined, namely Black Sea-Marmara, Black Sea, Marmara, Thrace, and Aegean sub-regions. To investigate the prevailing atmospheric circulation types (CTs) that cause precipitation occurrence and intensity in these five different rainfall sub-basins, objective Lamb weather type (LWT) methodology was applied to National Centers of Environmental Prediction (NCEP)/National Center for Atmospheric Research (NCAR) reanalysis of daily mean sea level pressure (MSLP) data. Precipitation occurrence suggested that wet CTs (i.e. N, NE, NW, and C) offer a high chance of precipitation in all sub-regions. For the eastern (western) part of the region, the high probability of rainfall occurrence is shown under the influence of E (SE, S, SW) atmospheric CTs. In terms of precipitation intensity, N and C CTs had the highest positive gradients in all the sub-basins of the Marmara. In addition, although Marmara and Black Sea sub-regions have the highest daily rainfall potential during NE types, high daily rainfall totals are recorded in all sub-regions except the Black Sea during NW types.</description><subject>Analysis</subject><subject>Aquatic Pollution</subject><subject>Atmosphere</subject><subject>Atmospheric circulation</subject><subject>Atmospheric Protection/Air Quality Control/Air Pollution</subject><subject>Atmospheric research</subject><subject>Atmospheric Sciences</subject><subject>Climatology</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>Marine</subject><subject>Original Paper</subject><subject>Precipitation</subject><subject>Rain</subject><subject>Studies</subject><subject>Waste Water Technology</subject><subject>Water Management</subject><subject>Water Pollution Control</subject><subject>Weather</subject><issn>0177-798X</issn><issn>1434-4483</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><recordid>eNp1kU1rFTEUhoNY8Fr9Ae4CbtrF1HxOMstS_ChUhfYW3YU0c3Kbdu5kTDLg_fdmHBdWkEC-eJ5wcl6E3lByRglR73KdiGgIlQ1tJW_oM7ShgotGCM2fow2hSjWq099foJc5PxBCWNuqDXrc3gMOox9mGB3g6LEt-5ine0jBYReSmwdbQhxxOUyQcd0k2NWzHfBkS4E05sWaErgwhbKyYcSfbdrbZPHJl294O6dHOJy-QkfeDhle_1mP0e2H99uLT83V14-XF-dXjRNal6bn-q71QlPte9l7zxjh8k7yVnEFvddOgBRApVJge8JIVykARzljTjum-DE6Wd-dUvwxQy5mH7KDYbAjxDkbqlvNieTdgr79B32Ic6qf-01JViFKK3W2Ujs7gKndiiVZV0cP--DiCD7U-3MpSUcVo10VTp8IlSnws-zsnLO5vLl-ytKVdSnmnMCbKYXauoOhxCzZmjVbU7M1S7ZmKYitTq7suIP0V9n_lX4BYC2l9Q</recordid><startdate>20170201</startdate><enddate>20170201</enddate><creator>Baltacı, H.</creator><creator>Kındap, T.</creator><creator>Ünal, A.</creator><creator>Karaca, M.</creator><general>Springer Vienna</general><general>Springer</general><general>Springer Nature B.V</general><scope>AAYXX</scope><scope>CITATION</scope><scope>ISR</scope><scope>3V.</scope><scope>7QH</scope><scope>7TG</scope><scope>7TN</scope><scope>7UA</scope><scope>7XB</scope><scope>88I</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>L6V</scope><scope>M2P</scope><scope>M7S</scope><scope>P5Z</scope><scope>P62</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>PTHSS</scope><scope>Q9U</scope></search><sort><creationdate>20170201</creationdate><title>The influence of atmospheric circulation types on regional patterns of precipitation in Marmara (NW Turkey)</title><author>Baltacı, H. ; 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Daily values of winter precipitation data based on 19 meteorological stations were used for the period from 1960 to 2012. Five clusters of coherent zones were determined, namely Black Sea-Marmara, Black Sea, Marmara, Thrace, and Aegean sub-regions. To investigate the prevailing atmospheric circulation types (CTs) that cause precipitation occurrence and intensity in these five different rainfall sub-basins, objective Lamb weather type (LWT) methodology was applied to National Centers of Environmental Prediction (NCEP)/National Center for Atmospheric Research (NCAR) reanalysis of daily mean sea level pressure (MSLP) data. Precipitation occurrence suggested that wet CTs (i.e. N, NE, NW, and C) offer a high chance of precipitation in all sub-regions. For the eastern (western) part of the region, the high probability of rainfall occurrence is shown under the influence of E (SE, S, SW) atmospheric CTs. In terms of precipitation intensity, N and C CTs had the highest positive gradients in all the sub-basins of the Marmara. In addition, although Marmara and Black Sea sub-regions have the highest daily rainfall potential during NE types, high daily rainfall totals are recorded in all sub-regions except the Black Sea during NW types.</abstract><cop>Vienna</cop><pub>Springer Vienna</pub><doi>10.1007/s00704-015-1653-1</doi><tpages>10</tpages></addata></record> |
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subjects | Analysis Aquatic Pollution Atmosphere Atmospheric circulation Atmospheric Protection/Air Quality Control/Air Pollution Atmospheric research Atmospheric Sciences Climatology Earth and Environmental Science Earth Sciences Marine Original Paper Precipitation Rain Studies Waste Water Technology Water Management Water Pollution Control Weather |
title | The influence of atmospheric circulation types on regional patterns of precipitation in Marmara (NW Turkey) |
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