4.5 Article

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

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JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES
卷 119, 期 7, 页码 1297-1308

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AMER GEOPHYSICAL UNION
DOI: 10.1002/2013JG002489

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资金

  1. National Science Council (NSC) of Taiwan [NSC 98-2221-E-002-198-]
  2. National Taiwan University [102R7604-2]
  3. Bill Lane Center for the American West
  4. Morrison Institute of Population and Resource Studies
  5. Phi Beta Kappa Northern California Association
  6. Stanford Biology SCORE Program
  7. NSF DDIG Program
  8. NOAA Climate and Global Change Postdoctoral Fellowship

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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 (Populus tremuloides 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-induced mortality 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.

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