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Intensity of tropical cyclones during pre and post monsoon seasons in relation to accumulated tropical heat potential over Bay of Bengal

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Intensity of tropical cyclones during pre and post monsoon seasons in relation to accumulated tropical heat potential over Bay of Bengal. / Vissa, Naresh Krishna; Satyanarayana, A. N. V.; Kumar, Bhaskaran Prasad .
In: Natural Hazards, Vol. 68, No. 2, 09.2013, p. 351-371.

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Vissa NK, Satyanarayana ANV, Kumar BP. Intensity of tropical cyclones during pre and post monsoon seasons in relation to accumulated tropical heat potential over Bay of Bengal. Natural Hazards. 2013 Sept;68(2):351-371. doi: 10.1007/s11069-013-0625-y

Author

Vissa, Naresh Krishna ; Satyanarayana, A. N. V. ; Kumar, Bhaskaran Prasad . / Intensity of tropical cyclones during pre and post monsoon seasons in relation to accumulated tropical heat potential over Bay of Bengal. In: Natural Hazards. 2013 ; Vol. 68, No. 2. pp. 351-371.

Bibtex

@article{a4b635b3afbf43df9cb9851ad1a04d2e,
title = "Intensity of tropical cyclones during pre and post monsoon seasons in relation to accumulated tropical heat potential over Bay of Bengal",
abstract = "The aim of the present study is to understand the impact of oceanic heat potential in relation to the intensity of tropical cyclones (TC) in the Bay of Bengal during the pre-monsoon (April–May) and post-monsoon (October–November) cyclones for the period 2006–2010. To accomplish this, the two-layer gravity model (TLGM) is employed to estimate daily tropical cyclone heat potential (TCHP) utilizing satellite altimeter data, satellite sea surface temperature (SST), and a high-resolution comprehensive ocean atlas developed for Indian Ocean, subsequently validated with in situ ARGO profiles. Accumulated TCHP (ATCHP) is estimated from genesis to the maximum intensity of cyclone in terms of minimum central pressure along their track of all the cyclones for the study period using TLGM generated TCHP and six-hourly National Centre for Environmental Prediction Climate Forecast System Reanalysis data. Similarly, accumulated sea surface heat content (ASSHC) is estimated using satellite SST. In this study, the relationship between ATCHP and ASSHC with the central pressure (CP) which is a function of TC intensity is developed. Results reveal a distinct relationship between ATCHP and CP during both the seasons. Interestingly, it is seen that requirement of higher ATCHP during pre-monsoon cyclones is required to attain higher intensity compared to post-monsoon cyclones. It is mainly attributed to the presence of thick barrier layer (BL) resulting in higher enthalpy fluxes during post-monsoon period, where as such BL is non-existent during pre-monsoon period.",
keywords = "Tropical cyclones, tropical cyclone heat potential, Barrier layer, ARGO",
author = "Vissa, {Naresh Krishna} and Satyanarayana, {A. N. V.} and Kumar, {Bhaskaran Prasad}",
year = "2013",
month = sep,
doi = "10.1007/s11069-013-0625-y",
language = "English",
volume = "68",
pages = "351--371",
journal = "Natural Hazards",
issn = "0921-030X",
publisher = "Springer Netherlands",
number = "2",

}

RIS

TY - JOUR

T1 - Intensity of tropical cyclones during pre and post monsoon seasons in relation to accumulated tropical heat potential over Bay of Bengal

AU - Vissa, Naresh Krishna

AU - Satyanarayana, A. N. V.

AU - Kumar, Bhaskaran Prasad

PY - 2013/9

Y1 - 2013/9

N2 - The aim of the present study is to understand the impact of oceanic heat potential in relation to the intensity of tropical cyclones (TC) in the Bay of Bengal during the pre-monsoon (April–May) and post-monsoon (October–November) cyclones for the period 2006–2010. To accomplish this, the two-layer gravity model (TLGM) is employed to estimate daily tropical cyclone heat potential (TCHP) utilizing satellite altimeter data, satellite sea surface temperature (SST), and a high-resolution comprehensive ocean atlas developed for Indian Ocean, subsequently validated with in situ ARGO profiles. Accumulated TCHP (ATCHP) is estimated from genesis to the maximum intensity of cyclone in terms of minimum central pressure along their track of all the cyclones for the study period using TLGM generated TCHP and six-hourly National Centre for Environmental Prediction Climate Forecast System Reanalysis data. Similarly, accumulated sea surface heat content (ASSHC) is estimated using satellite SST. In this study, the relationship between ATCHP and ASSHC with the central pressure (CP) which is a function of TC intensity is developed. Results reveal a distinct relationship between ATCHP and CP during both the seasons. Interestingly, it is seen that requirement of higher ATCHP during pre-monsoon cyclones is required to attain higher intensity compared to post-monsoon cyclones. It is mainly attributed to the presence of thick barrier layer (BL) resulting in higher enthalpy fluxes during post-monsoon period, where as such BL is non-existent during pre-monsoon period.

AB - The aim of the present study is to understand the impact of oceanic heat potential in relation to the intensity of tropical cyclones (TC) in the Bay of Bengal during the pre-monsoon (April–May) and post-monsoon (October–November) cyclones for the period 2006–2010. To accomplish this, the two-layer gravity model (TLGM) is employed to estimate daily tropical cyclone heat potential (TCHP) utilizing satellite altimeter data, satellite sea surface temperature (SST), and a high-resolution comprehensive ocean atlas developed for Indian Ocean, subsequently validated with in situ ARGO profiles. Accumulated TCHP (ATCHP) is estimated from genesis to the maximum intensity of cyclone in terms of minimum central pressure along their track of all the cyclones for the study period using TLGM generated TCHP and six-hourly National Centre for Environmental Prediction Climate Forecast System Reanalysis data. Similarly, accumulated sea surface heat content (ASSHC) is estimated using satellite SST. In this study, the relationship between ATCHP and ASSHC with the central pressure (CP) which is a function of TC intensity is developed. Results reveal a distinct relationship between ATCHP and CP during both the seasons. Interestingly, it is seen that requirement of higher ATCHP during pre-monsoon cyclones is required to attain higher intensity compared to post-monsoon cyclones. It is mainly attributed to the presence of thick barrier layer (BL) resulting in higher enthalpy fluxes during post-monsoon period, where as such BL is non-existent during pre-monsoon period.

KW - Tropical cyclones

KW - tropical cyclone heat potential

KW - Barrier layer

KW - ARGO

U2 - 10.1007/s11069-013-0625-y

DO - 10.1007/s11069-013-0625-y

M3 - Journal article

VL - 68

SP - 351

EP - 371

JO - Natural Hazards

JF - Natural Hazards

SN - 0921-030X

IS - 2

ER -