For those of you who still trying to decide which session to submit your 
AGU abstract to I encurage you to consider this one (especially if you are 
using stable isotopes and are working in mountainous systems).  We had a 
great oral and poster session last year on a similar topic.

B41:    The World Is Not Flat: Isotopic Tools for Understanding 
Mountainous Terrain 


Description:    Mountains cover twenty percent of the earth’s surface, 
including much of the western United States. They contain many of the 
world’s most productive ecosystems and provide essential ecosystem 
services (e.g., as “water towers” to lower-lying, urban areas). However, 
we have a very poor understanding of ecological processes in mountainous 
areas, especially as they relate to climate. The reasons for this are two-
fold. First, ecological processes differ distinctly in mountainous terrain 
compared with “flat ground." These differences result partly from 
downslope movement of sediments and partly from rapid gravitational 
drainage of water and cold air. Second, many of the large-scale 
integration tools available for ecosystem studies, including especially 
flux measurements, are difficult to employ in complex terrain. It is 
sobering to consider that sites selected for the entire Ameriflux network, 
and more recently for NEON core sites, have been biased deliberately in 
favor of flat terrain.

What else can we use as integrative measurements of ecosystem function in 
the mountains? Stable isotope measurements can integrate over space and 
time. For example, isotopic composition of stream water provides 
information on hydrologic processes over entire watersheds. In addition, 
the isotopic composition of dissolved ions in the water provides new 
opportunities to assess biogeochemical cycles upslope. Recent studies have 
demonstrated that a similar approach may be applied to nocturnal cold-air 
drainage systems, focusing on the carbon isotope composition of respired 
CO2 collected from the upslope airshed. These integrative measurements 
provide new opportunities to parameterize and test simulation models in 
the absence of eddy-flux data. This session welcomes contributions that 
discuss isotopic tools for the analysis of ecosystem processes in 
mountainous terrain. 
 

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