R. P. Sharma’s research while affiliated with India Meteorological Department and other places

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Publications (3)


Rapid Weakening of Very Severe Cyclonic Storm ‘Lehar’ – A Case Study
  • Chapter

November 2017

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62 Reads

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2 Citations

R. P. Sharma

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A depression formed over south Andaman Sea on 23rd evening and it intensified into a cyclonic storm, Lehar in the early morning of 24 November 2013 near Latitude 10.0° N and longitude 95.0° E. Moving northwestward, it crossed Andaman and Nicobar Islands near Port Blair around 0000 UTC of 25 November as a severe cyclonic storm. On 25th morning, it emerged into southeast Bay of Bengal and moved west-northwestward, intensified into a very severe cyclonic storm in the early hours of 26 November. However, while moving west-northwestwards over westcentral Bay of Bengal, it rapidly weakened from 27th afternoon and crossed Andhra Pradesh coast close to south of Machilipatnam around 0830 UTC of 28 November 2013 as a depression.


Figure 1: Tracks of tropical cyclones (TCs) during 2003–2013 under consideration in study and (b) an example of calculation of landfall point forecast error based on 0000 UTC of 27 December, 2011 in case of cyclone, Thane. Blue line indicates the landfall point forecast error (distance between forecast landfall point and observed landfall point).
Figure 3: Landfall point forecast errors (LPEs) and (b) landfall time forecast errors (LTEs) of various NWP models used by IMD for TC forecasting over NIO during 2009–2013.
Figure 6: Average landfall point forecast error (LPE) and (b) average landfall time forecast error (LTE) for TCs crossing Tamil Nadu (TN)/Sri Lanka, Andhra Pradesh (AP), Bangladesh and Myanmar coasts.
Figure 7: Average landfall point forecast error (LPE) and (b) average landfall time forecast error (LTE) for D/DD, CS and SCS or higher intensity at the time of initialization of forecast.
Figure 8: Average landfall point forecast error (LPE) and (b) average landfall time forecast error (LTE) for TCs during pre-monsoon and post-monsoon seasons over the NIO based on data of 2003–2013.

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Evaluation of official tropical cyclone landfall forecast issued by India Meteorological Department
  • Article
  • Full-text available

June 2015

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648 Reads

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48 Citations

Journal of Earth System Science

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D P Nayak

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[...]

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B K Bandyopadhyay

India Meteorological Department (IMD) introduced the objective tropical cyclone (TC) track forecast valid for next 24 hrs over the North Indian Ocean (NIO) in 2003. It further extended the validity period up to 72 hrs in 2009. Here an attempt is made to evaluate the TC landfall forecast issued by IMD during 2003–2013 (11 years) by calculating the landfall point forecast error (LPE) and landfall time forecast error (LTE). The average LPE is about 67, 95, and 124 km and LTE is about 4, 7, and 2 hrs, respectively for 24, 48, and 72-hr forecasts over the NIO as a whole during 2009–2013. The accuracy of TC landfall forecast has been analysed with respect to basin of formation (Bay of Bengal, Arabian Sea, and NIO as a whole), specific regions of landfall, season of formation (pre-monsoon and post-monsoon seasons), intensity of TCs (cyclonic storm (CS), and severe cyclonic storm (SCS) or higher intensities) at the time of initiation of forecast and type of track of TCs (climatological/straight moving and recurving/looping type). The LPE is less over the BOB than over the AS for all forecast lengths up to 72 hrs. Similarly, the LPE is less during the post-monsoon season than during pre-monsoon season. The LPEs are less for climatologically moving/straight moving TCs than for the recurving/looping TCs. The LPE over the NIO has decreased at the rate of about 14.5 km/year during 2003–2013 for 24-hr forecasts. The LTE does not show any significant improvement for 24-hr forecast during the same period. There is significant decrease in LPE and LTE during 2009–2013 compared to 2003–2008 due to the modernisation programme of IMD. The 24-hr LPE and LTE have decreased from 157.5 to 66.5 km and 7.8 to 4.1 hrs, respectively. However, there is still scope for further reduction in 48 and 72-hr forecast errors over the NIO to about 50 and 100 km respectively based on the latest technology including aircraft reconnaissance, deployment of buoys, and assimilation of more observational data from satellite and Doppler weather radars, etc., in the numerical weather prediction (NWP) models during the next five years.

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Evaluation of official tropical cyclone track forecast over north Indian Ocean issued by India Meteorological Department

June 2013

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795 Reads

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146 Citations

Journal of Earth System Science

India Meteorological Department (IMD) introduced the objective tropical cyclone (TC) track forecast valid for next 24 hr over the north Indian Ocean (NIO) in 2003. It further extended the validity period up to 72 hr in 2009. Here an attempt is made to evaluate the TC track forecast issued by IMD during 2003–2011 (9 years) by calculating the direct position error (DPE) and skill in track forecast. The accuracy of TC track forecast has been analysed with respect to basin of formation (Bay of Bengal, Arabian Sea and NIO as whole), season of formation (pre-monsoon and post-monsoon seasons), intensity of TCs (cyclonic storm and severe cyclonic storm or higher intensities) and type of track of TCs (climatological/straight moving and recurving/looping type). The average DPE is about 140, 262 and 386 km and skill is about 27%, 39% and 50%, respectively for 24, 48 and 72 hr forecasts over the NIO as a whole during 2009–2011. Though the DPE is higher and skill is less as compared to those in northwest Pacific and north Atlantic Ocean, the rate of decrease (increase) in DPE (skill) is higher over the NIO in recent years. The DPE (skill) over the NIO has decreased (increased) at the rate of about 7.3 km (3%) per year during 2003–2011 for 24 hr forecasts.

Citations (3)


... A rapid drop in this tropical cyclone's intensity is observed between 1200 UTC November 27, 2013 and 0000 UTC November 28, 2013. Moving northwestward, it then rapidly weakened from a very severe cyclonic storm at 0600 UTC on 27th to depression at 0000 UTC on November 28, 2013 (75-25 kts within 18 h) over the west-central Bay of Bengal (BoB), as noted by Sharma and Mohapatra (2017). The tropical cyclone Lehar experienced a major weakening with an enhancement in the sea level pressure by 18 hPa during the last 12 h before the landfall. ...

Reference:

Genesis and rapid weakening of tropical cyclone Lehar (2013)
Rapid Weakening of Very Severe Cyclonic Storm ‘Lehar’ – A Case Study
  • Citing Chapter
  • November 2017

... However, Powell and Aberson (2001) did not found statistically significant improvement in the trend of landfall position errors. Mohapatra et al. (2015) evaluated the TC landfall forecasts issued by the India Meteorological Department from 2003 to 2013 and also found that the landfall position error was smaller than the track forecast error. Besides, significant improvements were observed in the 24-h landfall forecasting during 2009-13 compared to 2003-08. ...

Evaluation of official tropical cyclone landfall forecast issued by India Meteorological Department

Journal of Earth System Science

... In this context, satellite technology dramatically aids in the early detection and effective prediction of TCs worldwide. Operational forecasts (Mohapatra et al., 2013a(Mohapatra et al., , 2013b and numerical weather prediction (NWP) models (Mohanty et al., 2010;Osuri et al., 2012), as well as dynamical-statistical models (Kotal et al., 2008), face challenges in terms of predicting the intensity of TCs. Even the model's ability to predict the rapid intensification of TCs is less accurate (Mohapatra and Sharma, 2019). ...

Evaluation of official tropical cyclone track forecast over north Indian Ocean issued by India Meteorological Department

Journal of Earth System Science