Driving forces of land surface temperature anomalous changes in North America in 2002-2018.

• Main Authors: Yan, Yibo, Mao, Kebiao, Shi, Jiancheng, Piao, Shilong, Shen, Xinyi, Liu, Yungang, Ren, Hong-Li, Bao, Qing, Dozier, Jeff
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: eScholarship, University of California 2020
• Subjects: North Atlantic; North Atlantic oscillation; Alaska
• Online Access: https://escholarship.org/uc/item/01q2x8ng

The land surface temperature (LST) changes in North America are very abnormal recently, but few studies have systematically researched these anomalies from several aspects, especially the influencing forces. After reconstructing higher quality MODIS monthly LST data (0.05° * 0.05°) in 2002-2018, we analyzed the LST changes especially anomalous changes and their drivingforces in North America. Here we show that North America warmed at the rate of 0.02 °C/y. TheLST changes in three regions, including frigid region in the northwestern (0.12 °C/y), the west coast from 20°N-40°N (0.07 °C/y), and the tropics south of 20°N (0.04 °C/y), were extremely abnormal. The El Nino and La Nina were the main drivers for the periodical highest and lowest LST, respectively. The North Atlantic Oscillation was closed related to the opposite change of LST in the northeastern North America and the southeastern United States, and the warming trend of the Florida peninsula in winter was closely related to enhancement of the North Atlantic Oscillation index. The Pacific Decadal Oscillation index showed a positive correlation with the LST in most Alaska. Vegetation and atmospheric water vapor also had a profound influence on the LST changes, but it had obvious difference in latitude.