abstract: Using a numerical model of the regional atmospheric circulation WRF-ARW, evolution of a strong bora in winter, 2013 (December, 2-3) near the Southern coast of the Crimea was reproduced.The features of the wind speed and temperature fields that describe formation of intensive atmospheric near-surface airflow over the leeward slope of the mountain ridge are considered.According to the results of numerical simulations carried out at high temporal resolution, strong temporal variability of the wind 
journal: Physical Oceanography