2018
DOI: 10.1002/met.1734
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Impact of data assimilation and air−sea flux parameterization schemes on the prediction of cyclone Phailin over the Bay of Bengal using the WRF‐ARW model

Abstract: The present study investigates the impact of data assimilation for prediction of the landfalling cyclone Phailin (October 8–13, 2013) over the Bay of Bengal by using the Weather Research and Forecasting Advanced Research model and its 3D variational data assimilation system. The impact of the air−sea flux (ACF) parameterization scheme is also tested with an improved model initial condition. Nine experiments were conducted, six with and without data assimilation at three different initial conditions. Three more… Show more

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Cited by 16 publications
(4 citation statements)
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“…Figure b shows the model domains with topography. The model set‐up uses 35 vertical sigma levels, with higher resolution in the lowest 1 km and the model top at 10 hPa (Singh and Bhaskaran, ; Singh and Tyagi, ). Six CPSs of the ARW‐WRF model are used, namely the Grell‐3 (G3) scheme (Grell and Devenyi, ), the new Kain–Fritsch (KF) scheme (Kain, ), the old simplified Arakawa–Schubert (SAS4) scheme (Pan, ), the new simplified Arakawa–Schubert (SAS14) scheme (Han and Pan, ), the new simplified Arakawa–Schubert Hurricane Weather Research and Forecasting version (SAS84) scheme (Han and Pan, ) and the Tiedtke (TDK) scheme (Tiedtke, ; Zhang et al , 2011); other model physics are kept unchanged and are described in Table .…”
Section: Description Of the Modelmentioning
confidence: 99%
See 1 more Smart Citation
“…Figure b shows the model domains with topography. The model set‐up uses 35 vertical sigma levels, with higher resolution in the lowest 1 km and the model top at 10 hPa (Singh and Bhaskaran, ; Singh and Tyagi, ). Six CPSs of the ARW‐WRF model are used, namely the Grell‐3 (G3) scheme (Grell and Devenyi, ), the new Kain–Fritsch (KF) scheme (Kain, ), the old simplified Arakawa–Schubert (SAS4) scheme (Pan, ), the new simplified Arakawa–Schubert (SAS14) scheme (Han and Pan, ), the new simplified Arakawa–Schubert Hurricane Weather Research and Forecasting version (SAS84) scheme (Han and Pan, ) and the Tiedtke (TDK) scheme (Tiedtke, ; Zhang et al , 2011); other model physics are kept unchanged and are described in Table .…”
Section: Description Of the Modelmentioning
confidence: 99%
“…A tropical cyclone (TC) is one of the most destructive weather phenomena in coastal regions worldwide due to its association with strong winds, heavy rainfall and storm surges (Singh and Tyagi, ). The accurate prediction of strong wind and heavy rain due to these storms is challenging to atmospheric modellers.…”
Section: Introductionmentioning
confidence: 99%
“…However, in the past few decades a significant improvement has been observed in the forecast of intense tropical cyclones over the North Indian Ocean. This improvement due to the high-resolution atmospheric modeling system [14][15][16] with improved physical processes [17][18][19][20], advanced data assimilation techniques including good quality of observations [21][22][23][24][25][26][27][28][29][30][31][32]. Therefore, a modeling study is very important in a high resolution to forecast the intensity of the ESCS over Bay of Bengal region in an increasing intensity and life-period.…”
Section: Introductionmentioning
confidence: 99%
“…Mandal et al (2016) reported that mean track errors (MTEs) for different ICs on days 1-4 were less than 100 km for the prediction of extremely severe cyclonic storm (ESCS) Phailin over the BoB region. A recent study by Singh and Tyagi (2019) suggested that the predicted storm track error and intensity were reduced using the 3DVar technique and with parameterization of the air-sea flux scheme in the WRF model. A study by Singh and Bhaskaran (2018) suggested that high resolution and more frequent lateral boundary conditions with assimilation of conventional and satellite radiances provide a better forecast of BoB TCs.…”
Section: Introductionmentioning
confidence: 99%