newtheoryfornutrientcompeon,$ plant$traits,$and$improved

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For additional information, contact: Staff Member Title Institution or Organization (555) 555-1234 [email protected] climatemodeling.science.energy.gov/acme New Theory for Nutrient Compe22on, Plant Traits, and Improved Advec2on Improves ALM W.J. Riley, B. Ghimire, Q. Zhu, J.Y. Tang, C.D. Koven N and P are important controllers of terrestrial Cclimate feedbacks Current representaHons in ALM are poorly tested and numerically problemaHc Here, we synthesize results from three recently submiOed ACME supported publicaHons: Using a new method to represent mulHnutrient and mulHconsumer interacHons (ECA) PrognosHc leaf traits that control photosynthesis Plant root nutrient uptake traits Improved advecHve flux calculaHons These advances lead to improved esHmates of global carbon exchanges, NO 3 leaching, and N 2 O gas emissions. Objective Equilibrium Chemistry Approximation application for nutrient constraints (Tang and Riley 2013) Comparison with experimental manipulations and global observations using ILAMB Improved advective transport calculation Approach Global GPP biases reduced by 65% Improved ALM captures N and P addiHon experiments The parHHoning of ecosystem N losses to N 2 O and NO 3 has been dramaHcally improved Improvements depend on improved representaHons of nutrient compeHHon and advecHve fluxes Impact Ghimire, B., W. J. Riley, and C. D. Koven (2015a), submi&ed Biogeosciences. Zhu, Q., and W. J. Riley (2015), submi&ed Nature Climate Change. Zhu, Q., W. J. Riley, J. Y. Tang, and C. D. Koven (2015), Biogeosciences Discussion, 12, 40574106. Figure. Global GPP bias reduced by 65%. Energy and water variables also improved (Ghimire et al., submi@ed Biogeosciences). Figure. N losses in CLM4 and CLM4.5 shown to be poorly predicted by Houlton et al. (2015). Improved compeLLon and advecLon dramaLcally improves N loss predicLons (Zhu and Riley, submi@ed Nature Climate Change). Figure. ECA accurately predicts N and P ferLlizaLon responses in tropical systems (Zhu et al. 2015, Biogeosciences D)

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Page 1: NewTheoryforNutrientCompeon,$ Plant$Traits,$and$Improved

For additional information, contact:

Staff Member Title

Institution or Organization

(555) 555-1234 [email protected] climatemodeling.science.energy.gov/acme

New  Theory  for  Nutrient  Compe22on,  Plant  Traits,  and  Improved  Advec2on  

Improves  ALM   W.J.  Riley,  B.  Ghimire,  Q.  Zhu,  J.Y.  Tang,  C.D.  Koven  

•  N  and  P  are  important  controllers  of  terrestrial  C-­‐climate  feedbacks    

•  Current  representaHons  in  ALM  are  poorly  tested  and  numerically  problemaHc  

•  Here,  we  synthesize  results  from  three  recently  submiOed  ACME-­‐supported  publicaHons:  

•  Using  a  new  method  to  represent  mulH-­‐nutrient  and  mulH-­‐consumer  interacHons  (ECA)  

•  PrognosHc  leaf  traits  that  control  photosynthesis  •  Plant  root  nutrient  uptake  traits  •  Improved  advecHve  flux  calculaHons    

•  These  advances  lead  to  improved  esHmates  of  global  carbon  exchanges,  NO3

-­‐  leaching,  and  N2O  gas  emissions.  

Objective

•  Equilibrium Chemistry Approximation application for nutrient constraints (Tang and Riley 2013)

•  Comparison with experimental manipulations and global observations using ILAMB

•  Improved advective transport calculation

Approach

•  Global  GPP  biases  reduced  by  65%    •  Improved  ALM  captures  N  and  P  

addiHon  experiments  •  The  parHHoning  of  ecosystem  N  losses  

to  N2O  and  NO3-­‐  has  been  dramaHcally  

improved    •  Improvements  depend  on  improved  

representaHons  of  nutrient  compeHHon  and  advecHve  fluxes  

Impact

Ghimire,  B.,  W.  J.  Riley,  and  C.  D.  Koven  (2015a),  submi&ed  Biogeosciences.  Zhu,  Q.,  and  W.  J.  Riley  (2015),  submi&ed  Nature  Climate  Change.  Zhu,  Q.,  W.  J.  Riley,  J.  Y.  Tang,  and  C.  D.  Koven  (2015),  Biogeosciences  Discussion,  12,  

4057-­‐4106.  

Figure.  Global  GPP  bias  reduced  by  65%.  Energy  and  water  variables  also  improved  (Ghimire  et  al.,  submi@ed  Biogeosciences).  

Figure.  N  losses  in  CLM4  and  CLM4.5  shown  to  be  poorly  predicted  by  Houlton  et  al.  (2015).  Improved  compeLLon  and  advecLon  dramaLcally  improves  N  loss  predicLons  (Zhu  and  Riley,  submi@ed  Nature  Climate  Change).  

Figure.  ECA  accurately  predicts  N  and  P  ferLlizaLon  responses  in  tropical  systems  (Zhu  et  al.  2015,  Biogeosciences  D)