The influence of dusts on radiation and temperature over the eastern Asia with a regional climate model

Xin Liu; Shuyi Chen; Zijia Guo; Haijiang Zhou; Yonghang Chen; Yanming Kang; Qiong Liu; Guan Huang; Tongqiang Liu; Chunmei Chen; Qing He

doi:10.1016/j.scitotenv.2021.148351

The influence of dusts on radiation and temperature over the eastern Asia with a regional climate model

Sci Total Environ. 2021 Oct 20:792:148351. doi: 10.1016/j.scitotenv.2021.148351. Epub 2021 Jun 8.

Authors

Xin Liu¹, Shuyi Chen², Zijia Guo¹, Haijiang Zhou¹, Yonghang Chen³, Yanming Kang⁴, Qiong Liu⁵, Guan Huang¹, Tongqiang Liu¹, Chunmei Chen⁶, Qing He⁷

Affiliations

¹ College of Environmental Science and Engineering, Donghua University, Shanghai 201620, PR China.
² College of Engineering, China University of Geosciences, Wuhan 430074, PR China.
³ College of Environmental Science and Engineering, Donghua University, Shanghai 201620, PR China. Electronic address: yonghangchen@dhu.edu.cn.
⁴ College of Environmental Science and Engineering, Donghua University, Shanghai 201620, PR China. Electronic address: ymkang@dhu.edu.cn.
⁵ College of Environmental Science and Engineering, Donghua University, Shanghai 201620, PR China; Shanghai Institute of Pollution Control and Ecological Security, Shanghai 200092, PR China.
⁶ College of Civil Engineering and Architecture, Zhejiang Sci-Tech University, Hangzhou 310018, PR China.
⁷ Institute of Desert Meteorology China Meteorological Administration, Urumqi 830001, PR China.

PMID: 34147814
DOI: 10.1016/j.scitotenv.2021.148351

Abstract

In order to investigate the climate effects of dusts, a regional climate model (RegCM 4.6) with the dust scheme was used to simulate the direct radiative forcing and air temperature response at 2 m near surface of dusts over the eastern Asia. Two sets of experiments were conducted, one with and one without dust aerosols. The experiment covered the main dust occurrence months from March to May for 8 years (2011-2018), and the simulation results were evaluated against ground station, reanalysis and satellite data. The model captured the spatiotemporal distribution of dust AOD and mass loading over the eastern Asia. However, it tended to underestimate the dust AOD and mass loading over the downwind of the dust source region and the Taklimakan Desert, and overestimate them over the north Xinjiang. The direct net radiative forcing including shortwave and longwave was up to -20 W·m^-2 at the surface and -10 W·m^-2 at the TOA over the dust source region due to the dominant negative shortwave forcing. The only exception of positive forcing at the TOA was observed along the western boundaries of the Tibetan Plateau due to the semi-persistent ice and snow cover. The dusts tended to warm the atmosphere more than 18 W·m^-2 and cool the surface locally up to -0.7 °C. Among the 5 sub-areas, the largest averaged regional direct radiative forcing induced by dusts appeared over the central Inner Mongolia in May with the value of -3.0 ± 2.1, -12.2 ± 4.1 and 9.2 ± 4.4 W·m^-2 at the TOA, surface and in the atmosphere, respectively. The results indicated that the model simulation for dusts should be further improved and the dust effects should be included in the estimates of climate change over the eastern Asia.

Keywords: Dust aerosols; East Asia; Radiative forcing; RegCM; Temperature response.

MeSH terms

Air Pollutants* / analysis
Asia, Eastern
Dust* / analysis
Environmental Monitoring
Temperature

Substances

Air Pollutants
Dust