Evaluating the Impacts of Land Cover and Soil Texture Changes on Simulated Surface Wind and Temperature. Issue 9 (3rd September 2020)

• Record Type: Journal Article
• Authors: Fu, Donglei; Liu, Yuping; Li, Haizhi; Liu, Songtao; Li, Bo; Thapa, Samit; Yabo, Stephen; Sun, Xiazhong; Tang, Bo; Zuo, Jinxiang; Qi, Hong; Tian, Chongguo
• Is Part Of: Earth and space science. Volume 7:Issue 9(2020)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2020-09-03
• Subjects: dataset incorporation -- land cover -- soil texture -- WRF; Space sciences -- Periodicals; Geophysics -- Periodicals; 500.5
• DOI: 10.1029/2020EA001173
• Languages: English
• ISSNs: 2333-5084

Abstract

Abstract: In this study, Chinese Academy of Sciences land cover dataset (CAS_LC) and soil texture dataset (CAS_ST) as well as Tsinghua University land cover dataset (TU_LC) were incorporated into the Weather Research and Forecasting (WRF) model to evaluate the impacts of land cover and soil texture changes on the surface wind and air temperature as compared with outdated default datasets. Six modeling scenarios including single updating for the three new datasets, combined updating of new datasets (CAS_LC + CAS_ST, TU_LC + CAS_ST), and default datasets are designed. WRF simulations were conducted with three resolutions (9, 3, and 1 km) for the period of 14 July to 31 September 2017 over Harbin. Results of the 10‐m wind speed, 10‐m wind direction, and 2‐m air temperature (T2) were evaluated against WRF default datasets (WLS). Results show that TU_LC‐related simulations with lower mean absolute error (MAE) demonstrated the usefulness of this dataset in the wind speed simulation, while the changing soil texture exerted a limited effect on modeled wind. CAS_LC improved simulated wind direction and T2. Significant changes in the three variables were frequently induced by urban and built‐up land or water bodies related transformations. The 3‐km grid resolution was sufficient to reasonably simulate the surface winds and air temperature. The roughness length was a main factor disturbing the wind speed, while the land cover transformation was responsible for the changes in surface temperature and heat fluxes, thereby affecting T2 simulation. Key Points: Land cover transformation dominates wind speed and wind direction changes Land cover as well as soil texture transformations dominate temperature changes 3km resolution is optimal for wind condition simulation, however, 1km resolution favors temperature simulation