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Mesoscale atmospheric vortices in the Okhotskand Bering Seas: results of satellite multisensorstudy

机译:Okhotskand Bering Seas中的Mescle大气涡旋:卫星多思考结果的结果

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Winter mesoscale cyclones (MCs) are frequently formed over the northern AsianMarginal Seas. They are often associated with precipitation and severe windscausing ice drift and serious disturbance in fishery and transport operation at thesea. Mesocyclones are difficult to forecast because of their rapid evolution andmovement. Climatological occurrence of mesoscale vortices in various areas isstill poorly understood. They were investigated mainly in the Northern AtlanticOcean, as well as in Gulf of Alaska and the Japan Sea in the Pacific Ocean.Favorable conditions for their development are also in the Bering and OkhotskSeas and to the east of Kamchatka where MCs are frequently observed on satelliteimages. However, conventional network is here sparse and the publishedinformation on MCs is too limited. Thus the main sources of quantitative spatialdata to examine these systems are satellite observations and fields of geophysicalparameters retrieved from measurements conducted by various satellite sensors.The MCs were detected by screening Envisat ASAR archive images acquired overthe Northwest Pacific in 2002-2006. High-resolution ASAR images of selectedMCs were compared with satellite visible and infrared imagery, QuikSCAT-derivedwind fields, surface analysis and upper-air analysis as well as with Aqua AMSR-E-derived fields of total atmospheric water vapor content V, total cloud liquidwater content Q and wind speed W.
机译:冬季Mesoscale旋风(MCS)经常在北方南方北方海洋上形成。它们通常与降水和严重的风力冰漂移和渔业和传输操作的严重扰动相关。由于他们的快速进化和缓解,群体旋转克隆很难预测。在各个领域的Mesoscale漩涡的气候发生在isstill难以理解的各个领域。他们在北部阿拉斯加北部和太平洋的墨西哥湾和日本海域进行了调查。适用于其发展的良好条件也在白天和鄂霍次克斯坦和堪察加以东,在卫星上经常观察到MCS 。然而,传统网络在这里稀疏,MCS上的发布信息太有限。因此,要检查这些系统的定量SpatialDATA的主要来源是从各种卫星传感器进行的测量中检索的地球物理参数的卫星观测和地球物理分析的领域。通过筛选在2002 - 2006年西北太平洋地区获得的Envisat ASAR归档图像来检测MCS。将SelectSMCS的高分辨率ASAR图像与卫星可见光和红外图像,Quikscat-errivewind领域,表面分析和上空气分析以及总大气水蒸气含量V的Aqua AMSR-E-衍生领域进行比较,总云液水内容Q和风速W.

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