Journal
CLIMATE DYNAMICS
Volume 59, Issue 1-2, Pages 281-295Publisher
SPRINGER
DOI: 10.1007/s00382-021-06134-8
Keywords
Amazon rainforest; Heat wave; Drought; Extreme weather; Land-surface; South America
Categories
Funding
- Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [405664/2018-4]
Ask authors/readers for more resources
Observational records show that heat waves in Amazonia have become more frequent, longer, and more intense. Climate change and deforestation are two significant drivers of these trends. Heat waves in the Amazon rainforest are understudied due to limited surface observations. This study is the first to analyze heat extremes in the Amazon and the first in South America to explore extreme heat wave events and associated conditions. The results reveal that extreme drying and intensified wind patterns contribute to the compound effect on extreme heat waves, leading to extremely hot temperatures.
Heat waves in Amazonia have become more frequent, longer, and more intense according to observational records. Climate change and deforestation are two significant drivers of such trends. In the Amazon rainforest, heat waves are still an understudied issue, in part due to limited surface observations. To date, heat waves in central Amazon have been associated with the ITCZ northward migration in austral winter, weakening moisture influx through the South American Monsoon System. This study contributes to this topic by being the first Amazon-specific analysis of heat extremes and the first in South America to jointly explore extreme heat wave events and associated synoptic atmospheric and land surface conditions. Ten of the most extreme heat waves are identified in the Southeast of Amazonia, from Era-Interim (1979 to 2018) maximum daily temperature records. Dry conditions are measured from relative humidity and evaporative fraction anomalies at surface and vertically also using the Era-Interim data. In all 10 events an extreme drying signal co-occurs with extreme heat waves. Wind patterns and anomalies revealed a consistent easterly dry advection anomalously extending to Southeast Amazonia. In addition, an intensification of the northerly South Atlantic Anticyclone wind circulation reduced the influx of moisture to Southeast Amazon, namely linked to the South American Low Level Jet. These, together, contributed to a compound effect on the extreme heat waves under near-surface drying conditions, which escalated hot temperatures to extreme heat.
Authors
I am an author on this paper
Click your name to claim this paper and add it to your profile.
Reviews
Recommended
No Data Available