Fig. 4: Comparison of seasonal climatology of various atmospheric parameters in the WNP.
From: Mechanism driving stronger tropical cyclones in cooler autumn than the hottest summer
Climatology of (a, b) winds at 1000 hPa (Windsfc, m s−1), d, e near surface specific humidity computed at 1000 hPa (qa, g kg−1). g, h Near surface Air temperature computed at 1000 hPa (Ta, °C) during the summer (left column) and autumn (central column) seasons, for the period 2005–2020. Differences in (c) Windsfc (m s−1), f qa (m s−1) (i) Ta (°C) and (l) Tssc (°C) between the two seasons (autumn minus summer, right column).
