Representation of Arabian Peninsula summer climate in a regional atmospheric model using spectral nudging

Raju Attada, Ravi Kumar Kunchala, Hari Prasad Dasari, Sanikommu Sivareddy, Viswanadhapalli Yesubabu, Omar Knio, Ibrahim Hoteit

Research output: Contribution to journalArticlepeer-review

3 Scopus citations


This study assesses the performance of the Weather Research and Forecasting (WRF) model in simulating the Arabian Peninsula summer climate for the period 2001–2016. The European Centre for Medium range Weather Forecast (ECMWF) reanalysis is downscaled using WRF without (CTRL) and with the Spectral Nudging (SPN) method. Our results suggest that the noticeable cold biases in surface temperatures (mean, minimum, and maximum) over the Arabian Peninsula in CTRL are significantly reduced in SPN. The seasonal patterns of surface pressure, cloud cover, lower and upper tropospheric circulation, and mid-tropospheric anticyclone are also simulated more realistically with SPN. The evaluation of mean vertical profiles of dynamical and thermo-dynamical features over the Arabian Peninsula further confirms the enhanced simulations with SPN with respect to CTRL. Though SPN captures better the observed evolution of rainfall compared to that of CTRL, it produces a positive rainfall bias over the Southwestern Arabian Peninsula. Stronger vertical motions associated with the local topography enhance the higher water vapor loading, condenses in the upper layers, and results in excess amount of rainfall in SPN. Furthermore, with SPN, WRF is further able to better simulate the synoptic features of heat waves. Overall, SPN enhances WRF simulation skill of the horizontal structures and vertical profiles of the Arabian Peninsula summer climate by enforcing a better balance between the small and large scale features and associated feedbacks.
Original languageEnglish (US)
JournalTheoretical and Applied Climatology
StatePublished - Apr 15 2021

Bibliographical note

KAUST Repository Item: Exported on 2021-05-06
Acknowledged KAUST grant number(s): CRG
Acknowledgements: This research work was supported by the Office of Sponsored Research (OSR) at King Abdullah University of Science and Technology (KAUST) under the Competitive Research Grant (CRG) program Grant#UFR/1/3706-01-01 and by the Saudi Aramco Center for Marine Environmental Research at KAUST. All simulations were conducted on the KAUST Super Computational facility (SHAHEEN) supported by the KAUST Supercomputing Laboratory (KSL).

ASJC Scopus subject areas

  • Atmospheric Science


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