Trends in Summer Season Climate for Eastern Europe and Southern Russia in the Early 21st Century

<table class="table-group" id="tab3"><tr><td><table class="table"><tr><td class="thead-hr" colspan="2"><hr/></td></tr><tr><td align="left">Types of ECM associated with positive anomalies characteristics </td><td align="center">Types of ECM associated with negative anomalies characteristics </td></tr><tr><td align="center" colspan="2"><hr/></td></tr><tr><td align="center" colspan="2">Air temperature</td></tr><tr><td align="left">8ds, 12а, 13s, 4c, 3, 9а</td><td align="center">4b, 8а, 7bs, 2b, 8bs, 2c</td></tr><tr><td align="center" colspan="2"><hr/></td></tr><tr><td align="center" colspan="2">Precipitation </td></tr><tr><td align="left">8а, 4c, 8bs, 12bs, 7bs</td><td align="center">10а, 10b, 9а, 8ds, 13s, 3, 6, 7аs</td></tr><tr class="table-tr"><td colspan="2"><hr class="tbody-hr"/></td></tr></table></td></tr></table>

Elementary circulation mechanisms and anomalies of climatic parameters during the summer period (1900–2013).

Advances in Meteorology

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Table 3

Table 3: Trends in Summer Season Climate for Eastern Europe and Southern Russia in the Early 21st Century 