Open AccessEvaluating the Impacts of Land Cover and Soil Texture Changes on Simulated Surface Wind and Temperature
Author(s) -
Fu Donglei,
Liu Yuping,
Li Haizhi,
Liu Songtao,
Li Bo,
Thapa Samit,
Yabo Stephen,
Sun Xiazhong,
Tang Bo,
Zuo Jinxiang,
Qi Hong,
Tian Chongguo
Publication year - 2020
Publication title -
earth and space science
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.843
H-Index - 23
ISSN - 2333-5084
DOI - 10.1029/2020ea001173
Subject(s) - weather research and forecasting model , environmental science , wind speed , land cover , soil texture , roughness length , meteorology , texture (cosmology) , wind direction , atmospheric sciences , land use , computer science , geology , soil science , soil water , wind profile power law , geography , image (mathematics) , civil engineering , artificial intelligence , engineering
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to evaluate the impacts of land cover and soil texture changes on the surface wind and air temperature as compared with outdated default datasets.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.