TY - JOUR
T1 - Remote sensing of tundra gross ecosystem productivity and light use efficiency under varying temperature and moisture conditions
AU - Huemmrich, K. F.
AU - Gamon, J. A.
AU - Tweedie, C. E.
AU - Oberbauer, S. F.
AU - Kinoshita, G.
AU - Houston, S.
AU - Kuchy, A.
AU - Hollister, R. D.
AU - Kwon, H.
AU - Mano, M.
AU - Harazono, Y.
AU - Webber, P. J.
AU - Oechel, W. C.
N1 - Funding Information:
This research was funded through a grant from the International Arctic Research Center to JG and FH at the Desert Research Institute, Reno, Nevada. This work was also partially supported by the National Science Foundation Office of Polar Programs grants OPP-9907185 and OPP-9906692 to SFO and PJW, respectively. The authors wish to thank the field crews for all of their work: Erika Anderson, Spring Strahm, Michelle Perl, Leticia Sanchez, Chris Donovan, Joe Verfaillie, Rommel Zulueta, Jean Van Dalen, Christopher Anderson, Dustin Bronson, Andrew Johnson, Shawn Serbin, Camila Schwyzer, and Justine Shaw, and the Barrow Arctic Science Consortium for logistics support.
PY - 2010/3/15
Y1 - 2010/3/15
N2 - Satellite observations have shown greening trends in tundra in response to climate change, suggesting increases in productivity. To better understand the ability of remote sensing to detect climate impacts on tundra vegetation productivity, we applied a photosynthetic light use efficiency model to simulated climate change treatments of tundra vegetation. We examined changes in the Normalized Difference Vegetation Index (NDVI) and photosynthetic light use efficiency (ε) in experimental warming and moisture treatments designed to simulate climate change in northern Alaska. Plots were warmed either passively, using Open Top Chambers, or actively using electric heaters in the soil. In one set of plots water table depth was actively altered, while other plots were established in locations that were naturally wet or dry. Over two growing seasons, plot-level carbon flux and spectral reflectance measurements were collected, and the results were used to derive a light use efficiency model that could explore the effects of moisture and temperature treatments using remote sensing. Warming increased values of canopy greenness (NDVI) relative to control plots, this effect being more pronounced in wet plots than in dry plots. Light use efficiency (LUE), the relationship between absorbed photosynthetically active radiation (PAR) and gross ecosystem production (GEP), was consistent across warming treatments, growing season, subsequent years, and sites. However, LUE was affected by vegetation type, which varied with moisture; plots in naturally dry locations showed reduced light use efficiency relative to moist plots. Additionally moss exhibited reduced LUE relative to vascular plants. Understory moss production, not accounted for by the usual definition of the fraction of absorbed PAR (fAPAR), was found to be a significant part of total GEP, particularly in areas with low vascular plant cover. These results support the use of light use efficiency models driven by spectral reflectance for estimating GEP in tundra vegetation, provided effects of vegetation functional type (e.g. mosses versus vascular plants) and microtopography are considered.
AB - Satellite observations have shown greening trends in tundra in response to climate change, suggesting increases in productivity. To better understand the ability of remote sensing to detect climate impacts on tundra vegetation productivity, we applied a photosynthetic light use efficiency model to simulated climate change treatments of tundra vegetation. We examined changes in the Normalized Difference Vegetation Index (NDVI) and photosynthetic light use efficiency (ε) in experimental warming and moisture treatments designed to simulate climate change in northern Alaska. Plots were warmed either passively, using Open Top Chambers, or actively using electric heaters in the soil. In one set of plots water table depth was actively altered, while other plots were established in locations that were naturally wet or dry. Over two growing seasons, plot-level carbon flux and spectral reflectance measurements were collected, and the results were used to derive a light use efficiency model that could explore the effects of moisture and temperature treatments using remote sensing. Warming increased values of canopy greenness (NDVI) relative to control plots, this effect being more pronounced in wet plots than in dry plots. Light use efficiency (LUE), the relationship between absorbed photosynthetically active radiation (PAR) and gross ecosystem production (GEP), was consistent across warming treatments, growing season, subsequent years, and sites. However, LUE was affected by vegetation type, which varied with moisture; plots in naturally dry locations showed reduced light use efficiency relative to moist plots. Additionally moss exhibited reduced LUE relative to vascular plants. Understory moss production, not accounted for by the usual definition of the fraction of absorbed PAR (fAPAR), was found to be a significant part of total GEP, particularly in areas with low vascular plant cover. These results support the use of light use efficiency models driven by spectral reflectance for estimating GEP in tundra vegetation, provided effects of vegetation functional type (e.g. mosses versus vascular plants) and microtopography are considered.
KW - Arctic tundra
KW - CO flux
KW - Fraction of absorbed photosynthetically active radiation
KW - Gross ecosystem exchange
KW - Leaf area index
KW - Light use efficiency
KW - Mosses
KW - Normalized Difference Vegetation Index
KW - Reflectance
KW - Simulated environmental change
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U2 - 10.1016/j.rse.2009.10.003
DO - 10.1016/j.rse.2009.10.003
M3 - Article
AN - SCOPUS:74149089497
SN - 0034-4257
VL - 114
SP - 481
EP - 489
JO - Remote Sensing of Environment
JF - Remote Sensing of Environment
IS - 3
ER -