carbon fluxes over temperate asia

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CARBON FLUXES OVER TEMPERATE ASIA N K INDIRA, PS SWATHI, PETER RAYNER, MICHEL RAMONET AND VINOD K GAUR

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CARBON FLUXES OVER TEMPERATE ASIA. N K INDIRA, PS SWATHI, PETER RAYNER, MICHEL RAMONET AND VINOD K GAUR. and temperature. ANSWERS SOUGHT : How would future climate trends evolve in response to specified carbon emissions over a given period ? - PowerPoint PPT Presentation

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Page 1: CARBON FLUXES OVER TEMPERATE ASIA

CARBON FLUXES OVER TEMPERATE ASIA

N K INDIRA, PS SWATHI, PETER RAYNER, MICHEL RAMONET AND VINOD K GAUR

Page 2: CARBON FLUXES OVER TEMPERATE ASIA
Page 3: CARBON FLUXES OVER TEMPERATE ASIA

ANSWERS SOUGHT:• How would future climate trends evolve in response to

specified carbon emissions over a given period ?• How are we faring in achieving desired goals assuming

some agreed regulatory measures in place ?

and temperature

Page 4: CARBON FLUXES OVER TEMPERATE ASIA

C(X*,t*)=Fn(Xj,tj)[δj*] C(X*,t*)=F(Xj,tj) * G(X*,X,t*,t)C(X*,t*)

Page 5: CARBON FLUXES OVER TEMPERATE ASIA

Inverse mode

•CO2 net fluxesa priori estimation

xb ; var/cov P

Atmospheric transport

H

Atmos. Conc.simulated

ymodel

Observationsyo ; var/cov R

Atmospheric transport model

Forward mode

Sc - ( C V ) = ( C) t

Page 6: CARBON FLUXES OVER TEMPERATE ASIA

UNCERTAINTIES IN CARBON FLUX ESTIMATION

•UNCERTAINTIES IN TRANSPORT MODELS

• INADEQUATE CONCENTRATION OBSERVATIONS (GURNEY 2002)

Page 7: CARBON FLUXES OVER TEMPERATE ASIA

TransCom Regions

Page 8: CARBON FLUXES OVER TEMPERATE ASIA

The highest CO2 observatory in the worldProbably the only one powered by solar energy

Page 9: CARBON FLUXES OVER TEMPERATE ASIA
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ATMOSPH. CO2 CONCENTRATIONS AT HANLEATMOSPH. CO2 CONCENTRATIONS AT HANLEAND FLUX ESTIMATIONS FOR TEMERATE ASIAAND FLUX ESTIMATIONS FOR TEMERATE ASIA

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NETWORK DESIGN FOR IMPROVED NETWORK DESIGN FOR IMPROVED COCO22 FLUX ESTIMATIONS FLUX ESTIMATIONS

APPROACH: MINIMISATION OF THE TRACE OF THE COVARIANCES

C(S) -1 = C(So) -1 + JT C(D) -1 J

OF GLOBAL OR EGIONAL SUB-MATRICES USING THE GENETIC ALGORITHM.

Page 12: CARBON FLUXES OVER TEMPERATE ASIA
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FIGURE SHOWS GLOBAL TRACE METRIC AS A FUNCTION OF ONE ADDITIONAL STATION FIGURE SHOWS GLOBAL TRACE METRIC AS A FUNCTION OF ONE ADDITIONAL STATION TO THE NETWORK OF GURNEY (2004). THE NUMBERS SHOW THE LOCATION S TO THE NETWORK OF GURNEY (2004). THE NUMBERS SHOW THE LOCATION S CHOSEN BY GA FOR 1, 2 OR 5, STATION NETWORKS WHICH MATCHES THE SCORE BESTCHOSEN BY GA FOR 1, 2 OR 5, STATION NETWORKS WHICH MATCHES THE SCORE BEST.

Page 14: CARBON FLUXES OVER TEMPERATE ASIA

Stations numbered 5 are located by GA, +s are the stations originally chosen

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PROBLEMS

•REDUCTION/ ATTRIBUTION OF UNCERTAINTIES IN FLUX ESTIMATIONS BECAUSE OF

INADEQUATE DATA

• TENDENCY FOR OPTIMAL NETWORKS IDENTIFIED BY GA TO HAVE CLUSTERING OF

STATIONS

Page 17: CARBON FLUXES OVER TEMPERATE ASIA

C(D) = AT CT(D) + AN CN(D)

[ CT(D)i ]1/2 ~ 0.32 + (0.32/M) VARi q(i,t) [ CN(D)i ]1/2 ~ NPPi exp[(- (Pi - P*)/H]

Upper left figure represents the advective Cd

and the upper right , that due to PP. The lower left is the total effect