Browning of the landscape of interior Alaska based on 1986-2009 Landsat sensor NDVI

Author:

Baird Rebecca A.1,Verbyla David1,Hollingsworth Teresa N.2

Affiliation:

1. Department of Forest Sciences, University of Alaska Fairbanks, Fairbanks, AK 99775, USA.

2. Boreal Ecology Cooperative Research Unit, USDA Forest Service Pacific Northwest Research Station, Fairbanks, AK 99775, USA.

Abstract

We used a time series of 1986–2009 Landsat sensor data to compute the Normalized Difference Vegetation Index (NDVI) for 30 m pixels within the Bonanza Creek Experimental Forest of interior Alaska. Based on simple linear regression, we found significant (p < 0.05) declining trends in mean NDVI of three dominant landscape types of floodplains, lowlands, and uplands. At smaller patch sizes, similar declining trends occurred among topographic classes of north- and south-facing slopes and valley bottoms and among forest classes, including black spruce (Picea mariana (Mill.) B.S.P.). Significant positive trends in mean NDVI occurred only in areas that were recently burned, whereas wetlands had no significant trend. The greatest departure from the NDVI trend line occurred following the 2004 drought for all forest classes except black spruce, which dominates the coldest sites, and balsam poplar (Populus balsamifera L.), which occurs on low, moist terraces within the Tanana River floodplain. The consistent long-term declining trend at several spatial scales may be due to a regional climatic regime shift that occurred in the mid-1970s.

Publisher

Canadian Science Publishing

Subject

Ecology,Forestry,Global and Planetary Change

Reference47 articles.

1. Arctic Council and the International Arctic Science Committee (IASC). 2005. Impacts of a warming climate: Arctic Climate Impacts Assessment. Cambridge University Press, Cambridge, UK.

2. Baird, R.A. 2011. Spatial and temporal trends in vegetation index in the Bonanza Creek Experimental Forest, University of Alaska Fairbanks, Fairbanks, Alaska. M.S. thesis, University of Alaska Fairbanks, Fairbanks, Alaska.

3. Reduced growth of Alaskan white spruce in the twentieth century from temperature-induced drought stress

4. Reconstruction of Summer Temperatures in Interior Alaska from Tree-Ring Proxies: Evidence for Changing Synoptic Climate Regimes

5. Satellite observations of high northern latitude vegetation productivity changes between 1982 and 2008: ecological variability and regional differences

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