High atmospheric demand for water can limit forest carbon uptake and transpiration as severely as dry soil-Reference-Cited by-同舟云学术

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High atmospheric demand for water can limit forest carbon uptake and transpiration as severely as dry soil

Published:2016-09-28 Issue:18 Volume:43 Page:9686-9695
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys. Res. Lett.

Author:

Sulman Benjamin N.¹²³,Roman D. Tyler¹⁴,Yi Koong¹,Wang Lixin⁵,Phillips Richard P.²,Novick Kimberly A.¹

Affiliation:

1. School of Public and Environmental Affairs Indiana University Bloomington Indiana USA

2. Department of Biology Indiana University Bloomington Indiana USA

3. Program in Atmospheric and Oceanic Sciences, Department of Geosciences Princeton University Princeton New Jersey USA

4. U.S. Department of Agriculture, Forest Service Northern Research Station Grand Rapids Minnesota USA

5. Department of Earth Sciences Indiana University‐Purdue University at Indianapolis Indianapolis Indiana USA

Funder

U.S. Department of Energy

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016GL069416

Reference62 articles.

1. Temperature sensitivity of drought-induced tree mortality portends increased regional die-off under global-change-type drought

2. The contributions of land-use change, CO2 fertilization, and climate variability to the Eastern US carbon sink

3. A global overview of drought and heat-induced tree mortality reveals emerging climate change risks for forests

4. The roles of hydraulic and carbon stress in a widespread climate-induced forest die-off

5. Tree mortality predicted from drought-induced vascular damage

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