Ocean variability contributes to sandstorms in Northern China

Ocean variability contributes to sandstorms in Northern China
The super sandstorm in North China on March 15, 2021. Credit: Dong Yueming

Extreme events such as the "North China Super Sandstorms" in March 2021 have significant impacts on human life, socio-economics and agricultural production. In addition to local meteorological conditions, sea surface temperature (SST) variability in different ocean basins also contributes to sandstorm frequency through atmospheric teleconnection and wave trains. Therefore, it is of great significance to study the impact of SST variability in these ocean basins on dust activities in North China.

To this end, researchers led by Dr. Li Xichen from the Institute of Atmospheric Physics of the Chinese Academy of Sciences, collaborating with Dr. Li Jing from Peking University, have investigated the variability in dust activity in the Gobi Desert and North China from 1981 to 2021, and in particular, to explore the relative contributions of SST variability in North Atlantic, Tropical Pacific and sea ice concentration (SIC) in the Arctic to the spring dust activity in northeastern Asia. Results were published in Geophysical Research Letters.

"Positive North Atlantic SST anomalies, negative Tropical Pacific SST anomalies (analogous to La Nina), and anomalously low Arctic SIC in the previous summer can all contribute to dust generation in the Gobi Desert and its transport to north China by inducing more favorable local meteorological conditions," said Li Jing. The above teleconnection patterns can be explained by established mechanism in atmospheric dynamics.

"Among the three ocean basins, the Tropical Pacific SST variability has the greatest impact on dust in the Gobi Desert, whereas the North Atlantic SST variability is the most important in driving dust events in North China. Considering the observed SST variability, the Tropical Pacific has the greatest impact on both regions," said Li Xichen.

Ocean variability contributes to sandstorms in Northern China
Variability of different ocean basins contribute to sandstorms in the Gobi Desert and North China. The color of the arrow: contribution of ocean variability to spring dust activity fraction in the Gobi Desert and North China. The color of the fill in the box: ensemble mean forcing trend of the Community Atmosphere Model version 4. Credit: IAP

This study is expected to provide theoretical support to better understand the causes of the variability of dust activity in northeastern Asia and to improve the modeling and projection of dust activities in this region.

More information: Guanyu Liu et al, Impact of sea surface temperature variability at different ocean basins on dust activities in the Gobi Desert and North China, Geophysical Research Letters (2022). DOI: 10.1029/2022GL099821

Journal information: Geophysical Research Letters

Citation: Ocean variability contributes to sandstorms in Northern China (2022, August 1) retrieved 19 April 2024 from https://phys.org/news/2022-08-ocean-variability-contributes-sandstorms-northern.html
This document is subject to copyright. Apart from any fair dealing for the purpose of private study or research, no part may be reproduced without the written permission. The content is provided for information purposes only.

Explore further

Precipitation in Central Asia shaped by sea surface temperature over tropical Pacific and North Atlantic

4 shares

Feedback to editors