Spatiotemporal Variations of Evapotranspiration in Amazonia Using the Wavelet Phase Difference Analysis

被引:5
|
作者
Zhang, Juan [1 ,2 ]
Feng, Ziyang [1 ]
Niu, Jie [1 ,3 ]
Melack, John M. [4 ]
Zhang, Jin [1 ,5 ]
Qiu, Han [6 ]
Hu, Bill X. [7 ]
Riley, William J. [8 ]
机构
[1] Jinan Univ, Coll Life Sci & Technol, Guangzhou, Peoples R China
[2] Tianjin Normal Univ, Sch Geog & Environm Sci, Tianjin, Peoples R China
[3] Green Dev Inst Zhaoqing, Zhaoqing, Peoples R China
[4] Univ Calif Santa Barbara, Earth Res Inst, Santa Barbara, CA 93106 USA
[5] Hohai Univ, Yangtze Inst Conservat & Dev, State Key Lab Hydrol Water Resources & Hydraul En, Nanjing, Peoples R China
[6] Pacific Northwest Natl Lab, Joint Global Change Res Inst, College Pk, MD USA
[7] Univ Jinan, Sch Water Conservancy & Environm, Jinan, Peoples R China
[8] Lawrence Berkeley Natl Lab, Div Earth Sci, Berkeley, CA USA
关键词
evapotranspiration (ET); wavelet analysis; wavelet phase difference (WPD); Amazon basin; Budyko framework; LAND-SURFACE; SOIL-MOISTURE; FOREST; DYNAMICS; SEASON; DRY; DEFORESTATION; CLIMATE; FLUXES; GROWTH;
D O I
10.1029/2021JD034959
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The relationships and seasonal-to-annual variations among evapotranspiration (ET), precipitation (P), terrestrial water storage anomalies (TWSA), radiation (downward shortwave radiation, DSR), and phenology (leaf area index, LAI) are complex across the Amazon basin. To analyze how ET is controlled by these influencing factors, we used wavelet phase difference (WPD) to investigate the effects of P, TWSA, DSR, and LAI on ET at different spatiotemporal scales. The Amazon-scale averaged ET has strong correlations with these factors at the annual and multi-year periodicities. The patterns of WPDs have south-north and west-east divides due to the significant variation in climatic conditions. The results demonstrate that ET is mainly affected by water and energy availability while vegetation regulates both processes. The deep soil moisture/groundwater can provide strong subsidies to ET during the meteorological dry season in the water-limited area of Amazon. The WPD can well reflect the responses of ET to the variations of P, TWSA, DSR, and LAI, and the process of vegetation sustaining ET in the dry years in the water-limited area of the Amazon.
引用
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页数:19
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