海洋性大陆地形对夏季季节内振荡的影响：基于2020年9月个例的数值模拟分析

孔钰博, 周逸豪, 汪曙光

The influence of topography of Maritime Continent on the boreal summer intraseasonal oscillation: Numerical simulation analysis based on a case in September 2020

Yubo Kong, Yihao Zhou, Shuguang Wang

图5 印度洋（左列）和MC（右列）的平均日降水量（填色图，单位：mm·d-1）和850 hPa纬向风异常（等值线图，单位：m·s-1）时间?纬度平均图， (a， b) (c， d) (e， f)分别为观测、CNTL和No Topography试验

Fig.5 The time?latitude diagrams of Indian Ocean (80°~90°E) averaged daily precipitation (shading, unit: mm·d-1) and 850 hPa zonal wind anomaly (contours, unit: m·s-1) from (a) Observation, (c) CNTL, and (e) No topography; (b, d, f) are the same as in (a, c, e) but for Maritime Continent (110°~120°E)