A simplified GIS approach to modeling global leaf water isoscapes.

The stable hydrogen (delta(2)H) and oxygen (delta(18)O) isotope ratios of organic and inorganic materials record biological and physical processes through the effects of substrate isotopic composition and fractionations that occur as reactions proceed. At large scales, these processes can exhibit sp...

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Main Authors: Jason B West, Adam Sobek, James R Ehleringer
Format: Article
Language:English
Published: Public Library of Science (PLoS) 2008-06-01
Series:PLoS ONE
Online Access:http://europepmc.org/articles/PMC2413011?pdf=render
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author Jason B West
Adam Sobek
James R Ehleringer
author_facet Jason B West
Adam Sobek
James R Ehleringer
author_sort Jason B West
collection DOAJ
description The stable hydrogen (delta(2)H) and oxygen (delta(18)O) isotope ratios of organic and inorganic materials record biological and physical processes through the effects of substrate isotopic composition and fractionations that occur as reactions proceed. At large scales, these processes can exhibit spatial predictability because of the effects of coherent climatic patterns over the Earth's surface. Attempts to model spatial variation in the stable isotope ratios of water have been made for decades. Leaf water has a particular importance for some applications, including plant organic materials that record spatial and temporal climate variability and that may be a source of food for migrating animals. It is also an important source of the variability in the isotopic composition of atmospheric gases. Although efforts to model global-scale leaf water isotope ratio spatial variation have been made (especially of delta(18)O), significant uncertainty remains in models and their execution across spatial domains. We introduce here a Geographic Information System (GIS) approach to the generation of global, spatially-explicit isotope landscapes (= isoscapes) of "climate normal" leaf water isotope ratios. We evaluate the approach and the resulting products by comparison with simulation model outputs and point measurements, where obtainable, over the Earth's surface. The isoscapes were generated using biophysical models of isotope fractionation and spatially continuous precipitation isotope and climate layers as input model drivers. Leaf water delta(18)O isoscapes produced here generally agreed with latitudinal averages from GCM/biophysical model products, as well as mean values from point measurements. These results show global-scale spatial coherence in leaf water isotope ratios, similar to that observed for precipitation and validate the GIS approach to modeling leaf water isotopes. These results demonstrate that relatively simple models of leaf water enrichment combined with spatially continuous precipitation isotope ratio and climate data layers yield accurate global leaf water estimates applicable to important questions in ecology and atmospheric science.
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spelling doaj.art-32c3dcf2ba024a59825f9d743bd74e9c2022-12-21T23:26:14ZengPublic Library of Science (PLoS)PLoS ONE1932-62032008-06-0136e244710.1371/journal.pone.0002447A simplified GIS approach to modeling global leaf water isoscapes.Jason B WestAdam SobekJames R EhleringerThe stable hydrogen (delta(2)H) and oxygen (delta(18)O) isotope ratios of organic and inorganic materials record biological and physical processes through the effects of substrate isotopic composition and fractionations that occur as reactions proceed. At large scales, these processes can exhibit spatial predictability because of the effects of coherent climatic patterns over the Earth's surface. Attempts to model spatial variation in the stable isotope ratios of water have been made for decades. Leaf water has a particular importance for some applications, including plant organic materials that record spatial and temporal climate variability and that may be a source of food for migrating animals. It is also an important source of the variability in the isotopic composition of atmospheric gases. Although efforts to model global-scale leaf water isotope ratio spatial variation have been made (especially of delta(18)O), significant uncertainty remains in models and their execution across spatial domains. We introduce here a Geographic Information System (GIS) approach to the generation of global, spatially-explicit isotope landscapes (= isoscapes) of "climate normal" leaf water isotope ratios. We evaluate the approach and the resulting products by comparison with simulation model outputs and point measurements, where obtainable, over the Earth's surface. The isoscapes were generated using biophysical models of isotope fractionation and spatially continuous precipitation isotope and climate layers as input model drivers. Leaf water delta(18)O isoscapes produced here generally agreed with latitudinal averages from GCM/biophysical model products, as well as mean values from point measurements. These results show global-scale spatial coherence in leaf water isotope ratios, similar to that observed for precipitation and validate the GIS approach to modeling leaf water isotopes. These results demonstrate that relatively simple models of leaf water enrichment combined with spatially continuous precipitation isotope ratio and climate data layers yield accurate global leaf water estimates applicable to important questions in ecology and atmospheric science.http://europepmc.org/articles/PMC2413011?pdf=render
spellingShingle Jason B West
Adam Sobek
James R Ehleringer
A simplified GIS approach to modeling global leaf water isoscapes.
PLoS ONE
title A simplified GIS approach to modeling global leaf water isoscapes.
title_full A simplified GIS approach to modeling global leaf water isoscapes.
title_fullStr A simplified GIS approach to modeling global leaf water isoscapes.
title_full_unstemmed A simplified GIS approach to modeling global leaf water isoscapes.
title_short A simplified GIS approach to modeling global leaf water isoscapes.
title_sort simplified gis approach to modeling global leaf water isoscapes
url http://europepmc.org/articles/PMC2413011?pdf=render
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