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Phil. Trans. R. Soc. A (2011) 369, 137–160<br />

doi:10.1098/rsta.2010.0238<br />

Changes in <strong>the</strong> <strong>potential</strong> distribution of humid<br />

tropical <strong>for</strong>ests on a warmer planet<br />

BY PRZEMYSLAW ZELAZOWSKI 1,∗ ,YADVINDER MALHI 1 ,<br />

CHRIS HUNTINGFORD 2 ,STEPHEN SITCH 3 AND JOSHUA B. FISHER 4<br />

1 Environmental Change Institute, School of Geography <strong>and</strong> <strong>the</strong> Environment,<br />

University of Ox<strong>for</strong>d, Ox<strong>for</strong>d OX1 3QY, UK<br />

2 Centre <strong>for</strong> Ecology <strong>and</strong> Hydrology, Walling<strong>for</strong>d OX10 8BB, UK<br />

3 School of Geography, University of Leeds, Leeds LS2 9JT, UK<br />

4 NASA Jet Propulsion Laboratory, Cali<strong>for</strong>nia Institute of Technology,<br />

Pasadena, CA 91109, USA<br />

The future of tropical <strong>for</strong>ests has become one of <strong>the</strong> iconic issues in climate-change<br />

science. A number of studies that have explored this subject have tended to focus on<br />

<strong>the</strong> output from one or a few climate models, which work at low spatial resolution,<br />

whereas society <strong>and</strong> conservation-relevant assessment of <strong>potential</strong> impacts requires<br />

a finer scale. This study focuses on <strong>the</strong> role of climate on <strong>the</strong> current <strong>and</strong> future<br />

distribution of humid tropical <strong>for</strong>ests (HTFs). We first characterize <strong>the</strong>ir contemporary<br />

climatological niche using annual rainfall <strong>and</strong> maximum climatological water stress,<br />

which also adequately describe <strong>the</strong> current distribution of o<strong>the</strong>r biomes within <strong>the</strong><br />

tropics. As a first-order approximation of <strong>the</strong> <strong>potential</strong> extent of HTFs in future climate<br />

regimes defined by <strong>global</strong> warming of 2 ◦ C <strong>and</strong> 4 ◦ C, we investigate changes in <strong>the</strong> niche<br />

through a combination of climate-change anomaly patterns <strong>and</strong> higher resolution (5 km)<br />

maps of current climatology. The climate anomalies are derived using data from 17<br />

coupled Atmosphere–Ocean General Circulation Models (AOGCMs) used in <strong>the</strong> <strong>Four</strong>th<br />

Assessment of <strong>the</strong> Intergovernmental Panel <strong>for</strong> Climate Change. Our results confirm<br />

some risk of <strong>for</strong>est retreat, especially in eastern Amazonia, Central America <strong>and</strong> parts of<br />

Africa, but also indicate a <strong>potential</strong> <strong>for</strong> expansion in o<strong>the</strong>r regions, <strong>for</strong> example around<br />

<strong>the</strong> Congo Basin. The finer spatial scale enabled <strong>the</strong> depiction of <strong>potential</strong> resilient<br />

<strong>and</strong> vulnerable zones with practically useful detail. We fur<strong>the</strong>r refine <strong>the</strong>se estimates<br />

by considering <strong>the</strong> impact of new environmental regimes on plant water dem<strong>and</strong> using<br />

<strong>the</strong> UK Met Office l<strong>and</strong>-surface scheme (of <strong>the</strong> HadCM3 AOGCM). The CO2-related<br />

reduction in plant water dem<strong>and</strong> lowers <strong>the</strong> risk of die-back <strong>and</strong> can lead to possible niche<br />

∗ Author <strong>for</strong> correspondence (przemyslaw.zelazowski@ouce.ox.ac.uk).<br />

Electronic supplementary material is available at http://dx.doi.org/10.1098/rspa.2010.0238 or via<br />

http://rspa.royalsocietypublishing.org.<br />

One contribution of 13 to a Theme Issue ‘<strong>Four</strong> <strong>degrees</strong> <strong>and</strong> <strong>beyond</strong>: <strong>the</strong> <strong>potential</strong> <strong>for</strong> a <strong>global</strong><br />

temperature increase of four <strong>degrees</strong> <strong>and</strong> its implications’.<br />

137<br />

This journal is © 2011 The Royal Society

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