Evaluation of WRF Simulations With Different Selections of Subgrid Orographic Drag Over the Tibetan Plateau. Issue 18 (29th September 2017)

• Record Type: Journal Article
• Authors: Zhou, X.; Beljaars, A.; Wang, Y.; Huang, B.; Lin, C.; Chen, Y.; Wu, H.
• Is Part Of: Journal of geophysical research. Volume 122:Issue 18(2017)
• Page Start: 9759
• Page End: 9772
• Publication Date: 2017-09-29
• Subjects: subgrid drag -- gravity wave drag -- flow blocking -- turbulent orographic form drag -- Tibetan Plateau -- WRF; Atmospheric physics -- Periodicals; Geophysics -- Periodicals; 551.5
• DOI: 10.1002/2017JD027212
• Languages: English
• ISSNs: 2169-897X

Abstract

Abstract: Weather Research and Forecasting (WRF) simulations with different selections of subgrid orographic drag over the Tibetan Plateau have been evaluated with observation and ERA‐Interim reanalysis. Results show that the subgrid orographic drag schemes, especially the turbulent orographic form drag (TOFD) scheme, efficiently reduce the 10 m wind speed bias and RMS error with respect to station measurements. With the combination of gravity wave, flow blocking and TOFD schemes, wind speed is simulated more realistically than with the individual schemes only. Improvements are also seen in the 2 m air temperature and surface pressure. The gravity wave drag, flow blocking drag, and TOFD schemes combined have the smallest station mean bias (−2.05°C in 2 m air temperature and 1.27 hPa in surface pressure) and RMS error (3.59°C in 2 m air temperature and 2.37 hPa in surface pressure). Meanwhile, the TOFD scheme contributes more to the improvements than the gravity wave drag and flow blocking schemes. The improvements are more pronounced at low levels of the atmosphere than at high levels due to the stronger drag enhancement on the low‐level flow. The reduced near‐surface cold bias and high‐pressure bias over the Tibetan Plateau are the result of changes in the low‐level wind components associated with the geostrophic balance. The enhanced drag directly leads to weakened westerlies but also enhances the a‐geostrophic flow in this case reducing (enhancing) the northerlies (southerlies), which bring more warm air across the Himalaya Mountain ranges from South Asia (bring less cold air from the north) to the interior Tibetan Plateau. Key Points: Subgrid orographic drag plays an important roles in the simulation of atmospheric flow The drag schemes obviously improve the dynamics over the complex Tibetan Plateau (TP) Improvements of TP air temperature and pressure due to subgrid orographic drag are associated with a modified geostrophic balance