Fig. 3: The spatial extension of Chl-a bloom for selected post-monsoon cyclones in BoB.
From: Tropical storms trigger phytoplankton blooms in the deserts of north Indian Ocean
The Chl-a averaged, overlaid with SSHA contours (solid—positive and dashed—negative), for 5 days before cyclone, during the entire cyclone period, five days just after the passage of cyclone and next 5 days for a Sidr (2007), b Madi (2013), and c Vardah (2016). The tracks of the respective cyclones are also shown.
