Water availability limits tree productivity, carbon stocks, and carbon residence time in mature forests across the western US

Water availability constrains the structure and function of terrestrial ecosystems and is projected to change in many parts of the world over the coming century. We quantified the response of tree net primary productivity (NPP), live biomass (BIO), and mean carbon residence time (CRT = BIO / NPP) to...

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Main Authors: L. T. Berner, B. E. Law, T. W. Hudiburg
Format: Article
Language:English
Published: Copernicus Publications 2017-01-01
Series:Biogeosciences
Online Access:http://www.biogeosciences.net/14/365/2017/bg-14-365-2017.pdf
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spelling doaj-af2e076672464fa8b441a81c9b15dc4c2020-11-25T00:34:20ZengCopernicus PublicationsBiogeosciences1726-41701726-41892017-01-0114236537810.5194/bg-14-365-2017Water availability limits tree productivity, carbon stocks, and carbon residence time in mature forests across the western USL. T. Berner0B. E. Law1T. W. Hudiburg2Department of Forest Ecosystems and Society, Oregon State University, 321 Richardson Hall, Corvallis, Oregon, OR 97331-2212, USADepartment of Forest Ecosystems and Society, Oregon State University, 321 Richardson Hall, Corvallis, Oregon, OR 97331-2212, USADepartment of Forest, Rangeland, and Fire Sciences, University of Idaho, 875 Perimeter Drive, Moscow, Idaho, ID 83844-1133, USAWater availability constrains the structure and function of terrestrial ecosystems and is projected to change in many parts of the world over the coming century. We quantified the response of tree net primary productivity (NPP), live biomass (BIO), and mean carbon residence time (CRT = BIO / NPP) to spatial variation in water availability in the western US. We used forest inventory measurements from 1953 mature stands (&gt; 100 years) in Washington, Oregon, and California (WAORCA) along with satellite and climate data sets covering the western US. We summarized forest structure and function in both domains along a 400 cm yr<sup>&minus;1</sup> hydrologic gradient, quantified with a climate moisture index (CMI) based on the difference between precipitation and reference evapotranspiration summed over the water year (October&ndash;September) and then averaged annually from 1985 to 2014 (CMI<sub><span style="text-decoration: overline">wy</span></sub>). Median NPP, BIO, and CRT computed at 10 cm yr<sup>&minus;1</sup> intervals along the CMI<sub><span style="text-decoration: overline">wy</span></sub> gradient increased monotonically with increasing CMI<sub><span style="text-decoration: overline">wy</span></sub> across both WAORCA (<i>r</i><sub>s</sub> = 0.93&ndash;0.96, <i>p</i> &lt; 0.001) and the western US (<i>r</i><sub>s</sub> = 0.93&ndash;0.99, <i>p</i> &lt; 0.001). Field measurements from WAORCA showed that median NPP increased from 2.2 to 5.6 Mg C ha<sup>&minus;1</sup> yr<sup>&minus;1</sup> between the driest and wettest 5 % of sites, while BIO increased from 26 to 281 Mg C ha<sup>&minus;1</sup> and CRT increased from 11 to 49 years. The satellite data sets revealed similar changes over the western US, though these data sets tended to plateau in the wettest areas, suggesting that additional efforts are needed to better quantify NPP and BIO from satellites in high-productivity, high-biomass forests. Our results illustrate that long-term average water availability is a key environmental constraint on tree productivity, carbon storage, and carbon residence time in mature forests across the western US, underscoring the need to assess potential ecosystem response to projected warming and drying over the coming century.http://www.biogeosciences.net/14/365/2017/bg-14-365-2017.pdf
collection DOAJ
language English
format Article
sources DOAJ
author L. T. Berner
B. E. Law
T. W. Hudiburg
spellingShingle L. T. Berner
B. E. Law
T. W. Hudiburg
Water availability limits tree productivity, carbon stocks, and carbon residence time in mature forests across the western US
Biogeosciences
author_facet L. T. Berner
B. E. Law
T. W. Hudiburg
author_sort L. T. Berner
title Water availability limits tree productivity, carbon stocks, and carbon residence time in mature forests across the western US
title_short Water availability limits tree productivity, carbon stocks, and carbon residence time in mature forests across the western US
title_full Water availability limits tree productivity, carbon stocks, and carbon residence time in mature forests across the western US
title_fullStr Water availability limits tree productivity, carbon stocks, and carbon residence time in mature forests across the western US
title_full_unstemmed Water availability limits tree productivity, carbon stocks, and carbon residence time in mature forests across the western US
title_sort water availability limits tree productivity, carbon stocks, and carbon residence time in mature forests across the western us
publisher Copernicus Publications
series Biogeosciences
issn 1726-4170
1726-4189
publishDate 2017-01-01
description Water availability constrains the structure and function of terrestrial ecosystems and is projected to change in many parts of the world over the coming century. We quantified the response of tree net primary productivity (NPP), live biomass (BIO), and mean carbon residence time (CRT = BIO / NPP) to spatial variation in water availability in the western US. We used forest inventory measurements from 1953 mature stands (&gt; 100 years) in Washington, Oregon, and California (WAORCA) along with satellite and climate data sets covering the western US. We summarized forest structure and function in both domains along a 400 cm yr<sup>&minus;1</sup> hydrologic gradient, quantified with a climate moisture index (CMI) based on the difference between precipitation and reference evapotranspiration summed over the water year (October&ndash;September) and then averaged annually from 1985 to 2014 (CMI<sub><span style="text-decoration: overline">wy</span></sub>). Median NPP, BIO, and CRT computed at 10 cm yr<sup>&minus;1</sup> intervals along the CMI<sub><span style="text-decoration: overline">wy</span></sub> gradient increased monotonically with increasing CMI<sub><span style="text-decoration: overline">wy</span></sub> across both WAORCA (<i>r</i><sub>s</sub> = 0.93&ndash;0.96, <i>p</i> &lt; 0.001) and the western US (<i>r</i><sub>s</sub> = 0.93&ndash;0.99, <i>p</i> &lt; 0.001). Field measurements from WAORCA showed that median NPP increased from 2.2 to 5.6 Mg C ha<sup>&minus;1</sup> yr<sup>&minus;1</sup> between the driest and wettest 5 % of sites, while BIO increased from 26 to 281 Mg C ha<sup>&minus;1</sup> and CRT increased from 11 to 49 years. The satellite data sets revealed similar changes over the western US, though these data sets tended to plateau in the wettest areas, suggesting that additional efforts are needed to better quantify NPP and BIO from satellites in high-productivity, high-biomass forests. Our results illustrate that long-term average water availability is a key environmental constraint on tree productivity, carbon storage, and carbon residence time in mature forests across the western US, underscoring the need to assess potential ecosystem response to projected warming and drying over the coming century.
url http://www.biogeosciences.net/14/365/2017/bg-14-365-2017.pdf
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