13 citations as recorded by crossref.

1. Role of convection in hydration of tropical UTLS: implication of AURA MLS long-term observations S. Jain et al. 10.5194/angeo-31-967-2013
2. Appearance of the persistently low tropopause temperature and ozone over the Bay of Bengal region S. Jain et al. 10.1007/s00703-017-0554-5
3. Further investigation on stratospheric air intrusion into the troposphere during the episode of tropical cyclone: Numerical simulation and MST radar observations S. Das et al. 10.1016/j.atmosres.2011.05.023
4. Temperature properties in the tropical tropopause layer and their correlations with Outgoing Longwave Radiation: FORMOSAT-3/COSMIC observations K. Wang et al. 10.1016/j.jastp.2017.07.012
5. Cloud-to-ground lightning and Mesoscale Convective Systems E. Mattos & L. Machado 10.1016/j.atmosres.2010.11.007
6. Convective tropopause over the tropics: Climatology, seasonality, and inter-annual variability inferred from long-term FORMOSAT-3/COSMIC-1 RO data S. Babu 10.1016/j.atmosres.2023.107159
7. Impact of monsoon‐associated deep‐penetrating clouds on the hydration of the tropical upper troposphere S. Jain et al. 10.1002/asl2.517
8. Tropopause height characteristics associated with ozone and stratospheric moistening during intense convective activity over Indian sub-continent B. Guha et al. 10.1016/j.gloplacha.2017.09.009
9. Seasonal and interannual variations of water vapor in the upper troposphere and lower stratosphere over the Asian Summer Monsoon region- in perspective of the tropopause and ocean-atmosphere interactions S. Das & K. Suneeth 10.1016/j.jastp.2020.105244
10. Occurrence of extremely low cold point tropopause temperature during summer monsoon season: ARMEX campaign and CHAMP and COSMIC satellite observations A. Jain et al. 10.1029/2010JD014340
11. Long-term variations in outgoing long-wave radiation (OLR), convective available potential energy (CAPE) and temperature in the tropopause region over India R. SAPRA et al. 10.1007/s12040-011-0113-2
12. AIRS observations of seasonal variability in meridional temperature gradient over Indian region at 100 hPa A. GUPTA et al. 10.1007/s12040-012-0254-y
13. Dry phase of tropical lower stratospheric water vapor: Role of BDC, convection and ozone variability S. Jain et al. 10.1016/j.jastp.2014.08.018