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Response of oceanic cyclogenesis metrics for NARGIS cyclone: a case study

Research output: Contribution to Journal/Magazine › Journal article › peer-review

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Response of oceanic cyclogenesis metrics for NARGIS cyclone: a case study. / Vissa, Naresh Krishna; Satyanarayana, A. N. V.; Kumar, Bhaskaran Prasad .
In: Atmospheric Science Letters, Vol. 14, No. 1, 2013, p. 7-13.

Research output: Contribution to Journal/Magazine › Journal article › peer-review

Harvard

Vissa, NK, Satyanarayana, ANV & Kumar, BP 2013, 'Response of oceanic cyclogenesis metrics for NARGIS cyclone: a case study', Atmospheric Science Letters, vol. 14, no. 1, pp. 7-13. https://doi.org/10.1002/asl2.407

APA

Vissa, N. K., Satyanarayana, A. N. V., & Kumar, B. P. (2013). Response of oceanic cyclogenesis metrics for NARGIS cyclone: a case study. Atmospheric Science Letters, 14(1), 7-13. https://doi.org/10.1002/asl2.407

Vancouver

Vissa NK, Satyanarayana ANV, Kumar BP. Response of oceanic cyclogenesis metrics for NARGIS cyclone: a case study. Atmospheric Science Letters. 2013;14(1):7-13. doi: 10.1002/asl2.407

Author

Vissa, Naresh Krishna ; Satyanarayana, A. N. V. ; Kumar, Bhaskaran Prasad . / Response of oceanic cyclogenesis metrics for NARGIS cyclone : a case study. In: Atmospheric Science Letters. 2013 ; Vol. 14, No. 1. pp. 7-13.

Bibtex

@article{34b7395b2dd643b287f129cdc1ab0a2c,
title = "Response of oceanic cyclogenesis metrics for NARGIS cyclone: a case study",
abstract = "In this study, variability of two oceanic cyclogenesis metrics, tropical cyclone heat potential (TCHP) and effective oceanic layer for cyclogenesis (EOLC) in the Bay of Bengal (BoB) during NARGIS cyclone is investigated. EOLC represents the geopotential thickness of near surface stratified layer forms because of the spread of low salinity waters due to fresh water influx from rivers and precipitation. Climatological fields of TCHP and EOLC reveal that NARGIS translated towards the region of higher EOLC as seen in the observations. A maximum daily sea surface cooling of 2 °C is observed along the right and rear side of NARGIS track.",
keywords = "tropical cyclone heat potential, effective oceanic layer for cyclogenesis, sea surface cooling",
author = "Vissa, {Naresh Krishna} and Satyanarayana, {A. N. V.} and Kumar, {Bhaskaran Prasad}",
note = "This is the publishers version of an article published in Atmospheric Science Letters, 14 (1), 2013. (c) Wiley Copyright 2013 Royal Meteorological Society",
year = "2013",
doi = "10.1002/asl2.407",
language = "English",
volume = "14",
pages = "7--13",
journal = "Atmospheric Science Letters",
issn = "1530-261X",
publisher = "John Wiley and Sons Inc.",
number = "1",

}

RIS

TY - JOUR

T1 - Response of oceanic cyclogenesis metrics for NARGIS cyclone

T2 - a case study

AU - Vissa, Naresh Krishna

AU - Satyanarayana, A. N. V.

AU - Kumar, Bhaskaran Prasad

N1 - This is the publishers version of an article published in Atmospheric Science Letters, 14 (1), 2013. (c) Wiley Copyright 2013 Royal Meteorological Society

PY - 2013

Y1 - 2013

N2 - In this study, variability of two oceanic cyclogenesis metrics, tropical cyclone heat potential (TCHP) and effective oceanic layer for cyclogenesis (EOLC) in the Bay of Bengal (BoB) during NARGIS cyclone is investigated. EOLC represents the geopotential thickness of near surface stratified layer forms because of the spread of low salinity waters due to fresh water influx from rivers and precipitation. Climatological fields of TCHP and EOLC reveal that NARGIS translated towards the region of higher EOLC as seen in the observations. A maximum daily sea surface cooling of 2 °C is observed along the right and rear side of NARGIS track.

AB - In this study, variability of two oceanic cyclogenesis metrics, tropical cyclone heat potential (TCHP) and effective oceanic layer for cyclogenesis (EOLC) in the Bay of Bengal (BoB) during NARGIS cyclone is investigated. EOLC represents the geopotential thickness of near surface stratified layer forms because of the spread of low salinity waters due to fresh water influx from rivers and precipitation. Climatological fields of TCHP and EOLC reveal that NARGIS translated towards the region of higher EOLC as seen in the observations. A maximum daily sea surface cooling of 2 °C is observed along the right and rear side of NARGIS track.

KW - tropical cyclone heat potential

KW - effective oceanic layer for cyclogenesis

KW - sea surface cooling

U2 - 10.1002/asl2.407

DO - 10.1002/asl2.407

M3 - Journal article

VL - 14

SP - 7

EP - 13

JO - Atmospheric Science Letters

JF - Atmospheric Science Letters

SN - 1530-261X

IS - 1

ER -