Carbon and water flux responses to physiology by environment interactions: a sensitivity analysis of variation in climate on photosynthetic and stomatal parameters

Sensitivity of carbon uptake and water use estimates to changes in physiology was determined with a coupled photosynthesis and stomatal conductance (g ₛ) model, linked to canopy microclimate with a spatially explicit scheme (MAESTRA). The sensitivity analyses were conducted over the range of intrasp...

Full description

Saved in:
Bibliographic Details
Published in:Climate dynamics Vol. 42; no. 9-10; pp. 2539 - 2554
Main Authors: Bauerle, William L, Daniels, Alex B, Barnard, David M
Format: Journal Article
Language:English
Published: Berlin/Heidelberg Springer-Verlag 01.05.2014
Springer Berlin Heidelberg
Springer
Springer Nature B.V
Subjects:
ISSN:0930-7575, 1432-0894
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:Sensitivity of carbon uptake and water use estimates to changes in physiology was determined with a coupled photosynthesis and stomatal conductance (g ₛ) model, linked to canopy microclimate with a spatially explicit scheme (MAESTRA). The sensitivity analyses were conducted over the range of intraspecific physiology parameter variation observed for Acer rubrum L. and temperate hardwood C₃ (C₃) vegetation across the following climate conditions: carbon dioxide concentration 200–700 ppm, photosynthetically active radiation 50–2,000 μmol m⁻² s⁻¹, air temperature 5–40 °C, relative humidity 5–95 %, and wind speed at the top of the canopy 1–10 m s⁻¹. Five key physiological inputs [quantum yield of electron transport (α), minimum stomatal conductance (g ₀), stomatal sensitivity to the marginal water cost of carbon gain (g ₁), maximum rate of electron transport (J ₘₐₓ), and maximum carboxylation rate of Rubisco (V cₘₐₓ)] changed carbon and water flux estimates ≥15 % in response to climate gradients; variation in α, J ₘₐₓ, and V cₘₐₓ input resulted in up to ~50 and 82 % intraspecific and C₃ photosynthesis estimate output differences respectively. Transpiration estimates were affected up to ~46 and 147 % by differences in intraspecific and C₃ g ₁ and g ₀ values—two parameters previously overlooked in modeling land–atmosphere carbon and water exchange. We show that a variable environment, within a canopy or along a climate gradient, changes the spatial parameter effects of g ₀, g ₁, α, J ₘₐₓ, and V cₘₐₓ in photosynthesis-g ₛ models. Since variation in physiology parameter input effects are dependent on climate, this approach can be used to assess the geographical importance of key physiology model inputs when estimating large scale carbon and water exchange.
Bibliography:http://dx.doi.org/10.1007/s00382-013-1894-6
SourceType-Scholarly Journals-1
ObjectType-Feature-1
content type line 14
ObjectType-Article-1
ObjectType-Feature-2
content type line 23
ISSN:0930-7575
1432-0894
DOI:10.1007/s00382-013-1894-6