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Research Detail

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Abdullah Al Mamun
Department of Physics, Khulna University of Engineering & Technology, Khulna, Bangladesh

M M Alam*
Department of Physics, Khulna University of Engineering & Technology, Khulna, Bangladesh

In the present study, the Weather Research and Forecast (WRF-ARW V3.5.1) model has been used to simulate the pre-monsoon temperature during 2010-2014 at different stations of Bangladesh. The model is run for 107 days for long-term prediction starting with the initial condition of 0000 UTC of 17 February up to 0000 UTC of 1 June during 2010-2014. The model is also run for 72-h with daily 0000 UTC initial conditions for 94 days for 24, 48, and 72-h lead-time prediction of temperature in the pre-monsoon season of 2014. 2m level simulated temperature data has been compared with the observed temperature of 33 meteorological stations of the Bangladesh Meteorological Department (BMD). The simulated monthly average temperature of March, April, and May 2014 for 24, 48, and 72-h prediction is found maximum in the western region whereas observed temperature is maximum in the SE region of the country. The correlation coefficient (CC) between observed and simulated temperature is found maximum for 24-h lead-time prediction in the month of March. As the time of the season progress and also the time of prediction are increased, the CC has decreased all over and this decrease is significant in the SE region of Bangladesh. The station distribution patterns of root mean square error (RMSE) and mean absolute error (MAE) are similar for 24, 48, 72 hours, and 92 days prediction but the MAE is lower than that of RMSE all through the country.  

  Microphysics; Cumulus Parameterization Scheme; Temperature; Pre-monsoon
  In Bangladesh
  00-00-2010
  00-00-2014
  Risk Management in Agriculture
  Temperature, Modeling

In this research, the WRF-ARW v3.5.1 model is used to simulate the pre-monsoon temperature during 2010- 2014 over Bangladesh and compare it with the daily observed temperature at different stations of BMD.

In the present study, the WRF-ARW model V3.5.1 has been used to simulate the monthly average temperature of 33 stations over Bangladesh in the pre-monsoon season. Final Reanalysis (FNL) (1ox1o ) data collected from National Centers for Environment Prediction (NCEP) is used as initial and Lateral Boundary Conditions (LBCs), which is updated at six hours interval i.e. the model is initialized with 0000, 0600, 1200, and 1800 UTC initial field of the corresponding date. The model has been configured in a single domain, 6 km horizontal grid spacing with 161×183 grids in the east-west and north-south directions and 30 vertical levels. In this research, the WSM6-class microphysics scheme coupling with the Kain-Fritsch cumulus parameterization scheme have been used. The model has been integrated by using initial and LBCs from NCEP-FNL analysis at six hourly intervals.

The model has been run 107 days for long-range prediction starting with the initial condition of 0000 UTC of 17 February up to 0000 UTC of 1 June for the period 2010-2014. The model is also run for 72-h with every day 0000 UTC initial conditions for 94 days starting with the initial condition of 0000 UTC of 27 February 2014 for the prediction of 24, 48, and 72-h lead time temperature in the month of March, April and May 2014. However, the results are presented for March-May to avoid the spin-up effects of the first 15 days. A spin-up period of 1 month may be sufficient for the atmospheric and upper soil layer, but it is not enough for deep soil layer variables (Christensen 1999). A great disparity in spin-up time between models, variables, and regions is often reported. Important reductions in spin-up time are expected in humid regions (Rodell et al. 2005) and, in particular, subtropical South America is a region where a quick equilibrium is expected (Silva and Berbery, 2006).

There is a limited number of meteorological observatories in the NE and SW regions of Bangladesh. Due to less number of stations in the NE and SW regions 8 more points have been added in the Bangladesh Map to study temperature data. 2m level temperature has been extracted at 3 hourly intervals then made daily and monthly average temperature data for 24, 48 and 72-h, and 92 days during the studied period. From the WRF Model run, 3 hourly outputs are made during the study period. These 3 hourly temperature data are converted into monthly temperature data of March, April, and May during 2010-2014. This simulated data has been compared with the observed temperature at 33 meteorological stations of BMD.

In this study, 24, 48, and 72-h have been considered as day 1, day 2, and day 3 of the model run. The monthly data has been plotted for March, April, and May using 24, 48, and 72-h lead-time prediction for the year 2014 and also using 92 days prediction during 2010-2014. The RMSE and MAE have been calculated for 33 meteorological stations because there is not any observational data for others. The CC, RMSE, and MAE for 24, 48, and 72-h and 92 days predicted temperature have been plotted using SURFER software for the year 2014.

  Journal of Engineering Science 08(1), 2017, 27-40
  
Funding Source:
1.   Budget:  
  

The station-wise simulated monthly average temperature of March, April and May 2014 for 24, 48 and 72- h prediction has been found maximum in the western region whereas observed temperature is found maximum in the central to SW region of the country. The distribution pattern of observed and model-simulated monthly average temperatures for 24, 48 and 72-hare almost similar all over Bangladesh except that the minimum values are predicted in the NE region but for observation, it is found in the NW region. The difference of observed and simulated monthly average temperatures lies within 1-2oC all over the country except SE region. The observed monthly average temperature is found minimum in the NW region but 92 days predicted temperature is found minimum in the S-SE and NE region and the difference lies within 5-6oC in the SE region. The CC between observed and simulated temperature is found maximum for 24-h lead-time prediction in the month of March. 92 days predicted monthly average temperature in May has been found maximum (minimum) in the W-NW (S-SE) region of the country whereas observed temperature is found maximum (minimum) in the SW (NE) regions. The pattern of simulated temperature is lower in the S-SE regions of Bangladesh due to the thermal inertia of the oceans that warms more slowly than land areas.

The RMSE of temperature for 92 days prediction is found minimum in the central region and increases in the surrounding areas of the country during the pre-monsoon season of 2010-2014. The RMSE of temperature lies within 1-2oC for the years 2010, 2011, 2012, and 2014 all over Bangladesh except the S-SE region of the country. The RMSE of temperature during March, April, and May 2013 is significantly higher with respect to that of 2010, 2011, 2012, and 2014 all over the country. The RMSE is found minimum for 24, 48 and 72 hours lead time prediction during March, April, and May of 2014 in the central to SW region and lies within 1oC and increases in the NW and SE regions. The RMSE has been found to increase as the prediction time increases from 24 to 72-h. The station-wise distribution patterns of RMSE and MAE are similar for 24, 48, 72 hours, and 92 days prediction but the MAE is lower than that of RMSE all through the country. For 24 hour lead time prediction of temperature in March 2014, the correlation coefficient (CC)is found greater than 0.92 all through except SE and NE regions. As the time of the season and prediction time has progressed, the CC decreases all over the country and this decrease is significant in the SE region of the country. WRF-ARW model is suitable for 24 to 72-lead time-temperature prediction. 24 hour lead time predicted temperatures are in good agreement with the observed temperatures.

  Journal
  


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