The development of the Novorossiysk bora on February 5–6, 2010 is simulated with high spatial and temporal resolution using the regional model of atmospheric circulation. Considered are typical features of the wind speed and air temperature fields. Singled out are two regimes defining the type of the air flowing around the mountain ridge and the temporal variability (gustiness) of the surface wind speed.
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Admiral Ushakov Maritime State Univ, Dept Theory & Hist State & Law, Vladivostok, RussiaAdmiral Ushakov Maritime State Univ, Dept Theory & Hist State & Law, Vladivostok, Russia
Abramyan, S. K.
Golubkina, K., V
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Admiral Ushakov Maritime State Univ, Dept Theory & Hist State & Law, Vladivostok, RussiaAdmiral Ushakov Maritime State Univ, Dept Theory & Hist State & Law, Vladivostok, Russia
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Texas A&M Univ, Coll Art & Sci, Dept Oceanog, College Stn, TX 77843 USATexas A&M Univ, Coll Art & Sci, Dept Oceanog, College Stn, TX 77843 USA
Lyu, Meng
Potter, Henry
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Texas A&M Univ, Coll Art & Sci, Dept Oceanog, College Stn, TX 77843 USATexas A&M Univ, Coll Art & Sci, Dept Oceanog, College Stn, TX 77843 USA
Potter, Henry
Collins, Clarence O.
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US Army Engineer Res & Dev Ctr, Coastal Observat & Anal Branch, Coastal & Hydraul Lab, Duck, NC USATexas A&M Univ, Coll Art & Sci, Dept Oceanog, College Stn, TX 77843 USA
Collins, Clarence O.
Yang, Xin
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Texas A&M Univ, Coll Art & Sci, Dept Oceanog, College Stn, TX 77843 USATexas A&M Univ, Coll Art & Sci, Dept Oceanog, College Stn, TX 77843 USA
Yang, Xin
Wang, Xiaoqi
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Texas A&M Univ, Coll Art & Sci, Dept Oceanog, College Stn, TX 77843 USATexas A&M Univ, Coll Art & Sci, Dept Oceanog, College Stn, TX 77843 USA