Variability in vertical structure of precipitation with sea surface temperature over the Arabian Sea and the Bay of Bengal as inferred by Tropical Rainfall Measuring Mission precipitation radar measurements

Saikranthi, Kadiri; Radhakrishna, Basivi; Narayana Rao, Thota; Satheesh, Sreedharan Krishnakumari

doi:https://doi.org/10.5194/acp-19-10423-2019

Articles | Volume 19, issue 15

https://doi.org/10.5194/acp-19-10423-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Special issue:

Interactions between aerosols and the South West Asian...

https://doi.org/10.5194/acp-19-10423-2019

© Author(s) 2019. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 19, issue 15

Research article

|

15 Aug 2019

Research article |

| 15 Aug 2019

Variability in vertical structure of precipitation with sea surface temperature over the Arabian Sea and the Bay of Bengal as inferred by Tropical Rainfall Measuring Mission precipitation radar measurements

Kadiri Saikranthi, Basivi Radhakrishna, Thota Narayana Rao, and Sreedharan Krishnakumari Satheesh

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Dec 2018	39	15	0	54
Jan 2019	37	7	0	44
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Apr 2019	27	8	0	35
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Jul 2019	20	5	0	25
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Oct 2019	41	15	0	56
Nov 2019	8	9	0	17
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Nov 2020	7	7	1	15
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Jan 2021	13	4	0	17
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Apr 2021	11	13	0	24
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Dec 2023	6	6	2	14
Jan 2024	7	2	1	10
Feb 2024	14	3	0	17
Mar 2024	15	9	2	26
Apr 2024	10	13	5	28
May 2024	17	6	2	25
Jun 2024	31	5	2	38
Jul 2024	41	11	0	52
Aug 2024	27	8	4	39
Sep 2024	11	4	0	15
Oct 2024	15	1	1	17
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Dec 2024	11	3	1	15

Cumulative views and downloads (calculated since 04 Sep 2018)

Month	HTML	PDF	XML	Total
Sep 2018	184	38	4	226
Oct 2018	75	7	1	83
Nov 2018	72	16	0	88
Dec 2018	39	15	0	54
Jan 2019	37	7	0	44
Feb 2019	29	6	0	35
Mar 2019	23	8	0	31
Apr 2019	27	8	0	35
May 2019	28	13	1	42
Jun 2019	16	6	0	22
Jul 2019	20	5	0	25
Aug 2019	256	51	5	312
Sep 2019	52	15	2	69
Oct 2019	41	15	0	56
Nov 2019	8	9	0	17
Dec 2019	16	8	0	24
Jan 2020	16	4	0	20
Feb 2020	12	6	1	19
Mar 2020	5	5	1	11
Apr 2020	11	3	0	14
May 2020	5	6	0	11
Jun 2020	16	10	0	26
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Dec 2020	7	7	0	14
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Mar 2021	10	7	0	17
Apr 2021	11	13	0	24
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Jun 2021	5	10	0	15
Jul 2021	9	17	0	26
Aug 2021	8	12	0	20
Sep 2021	9	10	0	19
Oct 2021	11	33	0	44
Nov 2021	8	28	2	38
Dec 2021	18	11	0	29
Jan 2022	10	10	0	20
Feb 2022	10	4	1	15
Mar 2022	7	6	0	13
Apr 2022	6	9	1	16
May 2022	3	3	0	6
Jun 2022	6	1	0	7
Jul 2022	15	4	0	19
Aug 2022	42	5	1	48
Sep 2022	22	0	22
Oct 2022	8	4	0	12
Nov 2022	8	6	0	14
Dec 2022	11	7	1	19
Jan 2023	9	6	0	15
Feb 2023	16	10	0	26
Mar 2023	14	5	1	20
Apr 2023	5	2	0	7
May 2023	4	6	0	10
Jun 2023	11	4	1	16
Jul 2023	12	10	1	23
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Dec 2023	6	6	2	14
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Feb 2024	14	3	0	17
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May 2024	17	6	2	25
Jun 2024	31	5	2	38
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Short summary

Recent studies have shown that simulation of monsoons can be improved with an exact representation of SST–precipitation relationship. The vertical structure of precipitation with SST is distinctly different over the Arabian Sea than over the Bay of Bengal. The reflectivity profiles show variation with SST over the Arabian Sea and do not show considerable variation with SST over the Bay of Bengal. The variations in reflectivity profiles seem to originate at the cloud formation stage itself.

Variability in vertical structure of precipitation with sea surface temperature over the Arabian Sea and the Bay of Bengal as inferred by Tropical Rainfall Measuring Mission precipitation radar measurements

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