GSTDTAP  > 气候变化
DOI10.1111/gcb.14445
Comparing optimal and empirical stomatal conductance models for application in Earth system models
Franks, Peter J.1; Bonan, Gordon B.2; Berry, Joseph A.3; Lombardozzi, Danica L.2; Holbrook, N. Michele4; Herold, Nicholas1; Oleson, Keith W.2
2018-12-01
发表期刊GLOBAL CHANGE BIOLOGY
ISSN1354-1013
EISSN1365-2486
出版年2018
卷号24期号:12页码:5708-5723
文章类型Article
语种英语
国家Australia; USA
英文摘要

Earth system models (ESMs) rely on the calculation of canopy conductance in land surface models (LSMs) to quantify the partitioning of land surface energy, water, and CO2 fluxes. This is achieved by scaling stomatal conductance, g(w), determined from physiological models developed for leaves. Traditionally, models for g(w) have been semi-empirical, combining physiological functions with empirically determined calibration constants. More recently, optimization theory has been applied to model g(w) in LSMs under the premise that it has a stronger grounding in physiological theory and might ultimately lead to improved predictive accuracy. However, this premise has not been thoroughly tested. Using original field data from contrasting forest systems, we compare a widely used empirical type and a more recently developed optimization-type g(w) model, termed BB and MED, respectively. Overall, we find no difference between the two models when used to simulate g(w) from photosynthesis data, or leaf gas exchange from a coupled photosynthesis-conductance model, or gross primary productivity and evapotranspiration for a FLUXNET tower site with the CLM5 community LSM. Field measurements reveal that the key fitted parameters for BB and MED, g(1B) and g(1M,) exhibit strong species specificity in magnitude and sensitivity to CO2, and CLM5 simulations reveal that failure to include this sensitivity can result in significant overestimates of evapotranspiration for high-CO2 scenarios. Further, we show that g(1B) and g(1M) can be determined from mean c(i)/c(a) (ratio of leaf intercellular to ambient CO2 concentration). Applying this relationship with c(i)/c(a) values derived from a leaf delta C-13 database, we obtain a global distribution of g(1B) and g(1M), and these values correlate significantly with mean annual precipitation. This provides a new methodology for global parameterization of the BB and MED models in LSMs, tied directly to leaf physiology but unconstrained by spatial boundaries separating designated biomes or plant functional types.


英文关键词Ball-Berry model canopy conductance CLM forest CO2 response land surface model scaling stomatal conductance stomatal conductance model
领域气候变化 ; 资源环境
收录类别SCI-E
WOS记录号WOS:000449650600011
WOS关键词CARBON-ISOTOPE DISCRIMINATION ; WATER-USE EFFICIENCY ; LEAF C-13 DISCRIMINATION ; COMMUNITY LAND MODEL ; ELEVATED CO2 ; PLANT-RESPONSES ; ATMOSPHERIC CO2 ; CLIMATE ; PHOTOSYNTHESIS ; DIOXIDE
WOS类目Biodiversity Conservation ; Ecology ; Environmental Sciences
WOS研究方向Biodiversity & Conservation ; Environmental Sciences & Ecology
引用统计
文献类型期刊论文
条目标识符http://119.78.100.173/C666/handle/2XK7JSWQ/16930
专题气候变化
资源环境科学
作者单位1.Univ Sydney, Sch Life & Environm Sci, Sydney, NSW, Australia;
2.Natl Ctr Atmospher Res, POB 3000, Boulder, CO 80307 USA;
3.Carnegie Inst Sci, Dept Global Ecol, Stanford, CA USA;
4.Harvard Univ, Dept Organism & Evolutionary Biol, Cambridge, MA 02138 USA
推荐引用方式
GB/T 7714
Franks, Peter J.,Bonan, Gordon B.,Berry, Joseph A.,et al. Comparing optimal and empirical stomatal conductance models for application in Earth system models[J]. GLOBAL CHANGE BIOLOGY,2018,24(12):5708-5723.
APA Franks, Peter J..,Bonan, Gordon B..,Berry, Joseph A..,Lombardozzi, Danica L..,Holbrook, N. Michele.,...&Oleson, Keith W..(2018).Comparing optimal and empirical stomatal conductance models for application in Earth system models.GLOBAL CHANGE BIOLOGY,24(12),5708-5723.
MLA Franks, Peter J.,et al."Comparing optimal and empirical stomatal conductance models for application in Earth system models".GLOBAL CHANGE BIOLOGY 24.12(2018):5708-5723.
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