Fig. 2: Composite analysis of lower atmospheric stability and moistening over the NBOB.
From: Aerosol processes perturb cloud trends over Bay of Bengal: observational evidence

The spatial distribution of composite median temperature at ~900 hPa (a, b), and RH at 1000 hPa (c, d) from AIRS during March to May (MAM). The left column is composite median for the period of 2005–2009 (a, c) and the right column is same for 2015–2019 (b, d), respectively. e The difference between recent and past years of the temperature and RH vertical profiles. f The association of median temperature (at different levels) and columnar AOD over the NBOB (black box) region. Standard deviation values are used for plotting the bounded line and error bars.