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  4. Vegetation, land surface brightness, and temperature dynamics after aspen forest die-off
 
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Vegetation, land surface brightness, and temperature dynamics after aspen forest die-off

Journal
Journal of Geophysical Research-Biogeosciences
Journal Volume
119
Journal Issue
7
Pages
1297-1308
Date Issued
2014
Author(s)
CHO-YING HUANG  
DOI
10.1002/2013jg002489
URI
http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=ORCID&SrcApp=OrcidOrg&DestLinkType=FullRecord&DestApp=WOS_CPL&KeyUT=WOS:000340543000003&KeyUID=WOS:000340543000003
http://scholars.lib.ntu.edu.tw/handle/123456789/385820
https://www.scopus.com/inward/record.uri?eid=2-s2.0-84961316155&doi=10.1002%2f2013JG002489&partnerID=40&md5=359678e2e8dbfba25738402ac266ff4f
Abstract
Forest dynamics following drought-induced tree mortality can affect regional climate through biophysical surface properties. These dynamics have not been well quantified, particularly at the regional scale, and are a large uncertainty in ecosystem-climate feedback. We investigated regional biophysical characteristics through time (1995-2011) in drought-impacted (2001-2003), trembling aspen (Populustremuloides Michx.) forests by utilizing Landsat time series green and brown vegetation cover, surface brightness (total shortwave albedo), and daytime land surface temperature.We quantified the temporal dynamics and postdrought recovery of these characteristics for aspen forests experiencing severe drought-induce dmortality in the San Juan National Forest in southwestern Colorado, USA. We partitioned forests into three categories from healthy to severe mortality (Healthy, Intermediate, and Die-off ) by referring to field observations of aspen canopy mortality and live aboveground biomass losses. The vegetation cover of die-off areas in 2011 (26.9%of the aspen forest) was significantly different compared to predrought conditions(decrease of 7.4% of the green vegetation cover and increase of 12.1% of the brown vegetation cover compared to 1999). The surface brightness of the study region 9 years after drought however was comparable to predrought estimates (12.7-13.7%). Postdrought brightness was potentially influenced by understory shrubs, since they became the top layer green canopies in disturbed sites from a satellite's point of view. Satellite evidence also showed that the differences of land surface temperature among the three groups increased substantially (≥45%) after drought, possibly due to the reduction of plant evapotranspiration in the Intermediate and Die-off sites. Our results suggest that the mortality-affected systems have not recovered in terms of the surface biophysical properties.We also find that the temporal dynamics of vegetation cover holds great potential for assessing propensity of subsequent mortality during drought itself, which could provide effective monitoring and potentially a much needed "early warning" of drought-induced tree mortality. © 2014. American Geophysical Union. All Rights Reserved.
SDGs

[SDGs]SDG13

[SDGs]SDG15

Other Subjects
aboveground biomass; biophysics; brightness temperature; climate feedback; evapotranspiration; land surface; Landsat; mortality; surface temperature; temporal analysis; time series; vegetation cover; Colorado; San Juan National Forest; United States
Type
journal article

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