4.7 Article

Seasonal and diurnal performance of daily forecasts with WRF V3.8.1 over the United Arab Emirates

Journal

GEOSCIENTIFIC MODEL DEVELOPMENT
Volume 14, Issue 3, Pages 1615-1637

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/gmd-14-1615-2021

Keywords

-

Funding

  1. UAE Research Program for Rain Enhancement Science, under the National Center of Meteorology, Abu Dhabi, UAE
  2. High Performance Computing Center Stuttgart (HLRS)

Ask authors/readers for more resources

The study shows that WRF performs well in predicting temperature and humidity parameters during the daytime in the UAE, with some nocturnal cold bias. There are varying degrees of biases for temperature (T-2m) and dew point (TD2m) in different regions, while wind speed (UV 10m) performance still needs improvement.
Effective numerical weather forecasting is vital in arid regions like the United Arab Emirates (UAE) where extreme events like heat waves, flash floods, and dust storms are severe. Hence, accurate forecasting of quantities like surface temperatures and humidity is very important. To date, there have been few seasonal-to-annual scale verification studies with WRF at high spatial and temporal resolution. This study employs a convection-permitting scale (2.7 km grid scale) simulation with WRF with Noah-MP, in daily forecast mode, from 1 January to 30 November 2015. WRF was verified using measurements of 2 m air temperature (T-2m), 2 m dew point (TD2m), and 10 m wind speed (UV10m) from 48 UAE WMO-compliant surface weather stations. Analysis was made of seasonal and diurnal performance within the desert, marine, and mountain regions of the UAE. Results show that WRF represents temperature (T-2m) quite adequately during the daytime with biases <= +1 degrees C. There is, however, a nocturnal cold bias (-1 to -4 degrees C), which increases during hotter months in the desert and mountain regions. The marine region has the smallest T-2m biases (< -0.75 degrees C). WRF performs well regarding TD2m, with mean biases mostly <= 1 degrees C. TD2m over the marine region is overestimated, though (0.75-1 degrees C), and nocturnal mountain TD2m is underestimated (similar to -2 degrees C). UV 10 m performance on land still needs improvement, and biases can occasionally be large (1-2 m s(-1)). This performance tends to worsen during the hot months, particularly inland with peak biases reaching similar to 3 m s(-1). UV10m is better simulated in the marine region (bias <= 1 m s(-1)). There is an apparent relationship between T-2m bias and UV10m bias, which may indicate issues in simulation of the daytime sea breeze. TD2m biases tend to be more independent. Studies such as these are vital for accurate assessment of WRF nowcasting performance and to identify model deficiencies. By combining sensitivity tests, process, and observational studies with seasonal verification, we can further improve forecasting systems for the UAE.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

No Data Available
No Data Available