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Fig 1 - West coast India’s rainfall is becoming more convective

Fig. 1 Interannual variability of LTT, SST, rainfall and OLR. a Interannual variability of anomalous sea surface tem-perature (SST) (°C, black) and lower tropospheric temperature (LTT: 1000 hPa to 700 hPa average) (°C, red) anomalies respectively over the Arabian sea (65-70 °E and 15-20 °N) and the western coast of India (73-77 °E and 8-20 °N) during JJAS. b Interannual variability of anomalous rainfall (mm.day −1 , Blue) and OLR(Wm −2 , Orange) anomalies, respectively, over the western coast of India (73-77 °E and 8-20 ° N) during JJAS. Fitted trends obtained by linear regression on year are indicated by dashed lines.
Interannual variability of LTT, SST, rainfall and OLR. a Interannual variability of anomalous sea surface tem-perature (SST) (°C, black) and lower tropospheric temperature (LTT: 1000 hPa to 700 hPa average) (°C, red) anomalies respectively over the Arabian sea (65-70 °E and 15-20 °N) and the western coast of India (73-77 °E and 8-20 °N) during JJAS. b Interannual variability of anomalous rainfall (mm.day −1 , Blue) and OLR(Wm −2 , Orange) anomalies, respectively, over the western coast of India (73-77 °E and 8-20 ° N) during JJAS. Fitted trends obtained by linear regression on year are indicated by dashed lines.
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