i nt roduct ion t o simcli m
play

I nt roduct ion t o SimCLI M Wei Ye The I nt er nat ional Global - PowerPoint PPT Presentation

I nt roduct ion t o SimCLI M Wei Ye The I nt er nat ional Global Change I nst it ut e Univer sit y of Waikat o What is SimCLI M? A resear ch pr oduct f r om New Zealand Climat e Change I mpact St udies (CLI MPACTS) An int egr at ed


  1. I nt roduct ion t o SimCLI M Wei Ye The I nt er nat ional Global Change I nst it ut e Univer sit y of Waikat o

  2. What is SimCLI M? • A resear ch pr oduct f r om New Zealand Climat e Change I mpact St udies (CLI MPACTS) • An int egr at ed comput er model f or climat e change impact assessment • Build-in cust omised GI S syst em t o suppor t mult i- level spat ial analysis • Based on I PCC guidelines and upgr adeable wit h lat est scient if ic r esear ch inf or mat ion.

  3. Why Develop int egrat ed assessment model ? Some Background: • Climat e change is REAL and it s impact has been f elt by people all over t he wor ld • High demand f rom t he st akeholder s t o include climat e change impact inf ormat ion int o t heir decision making

  4. Why Develop int egrat ed assessment model ? Some Background: • Model based approach have helped st udy t he global warming, it s impact and evaluat e t he possibilit y of mit igat ion and adapt at ion possibilit y in t he past and in t he f oreseeable f ut ure • GCMs are t he most comprehensive t ools f or est imat ing t he response of climat e t o r adiat ion f orcing • I t has been a challenge t o mainst ream such scient if ic inf ormat ion int o act ion, due t o t he uncer t aint ies of t he model and t he complexit y t o ref lect such uncert aint ies in policy-making process

  5. What is t he challenge? Uncert aint ies!!!

  6. What is t he challenge? • Uncert aint ies in f ut ure greenhouse gas and aerosol emissions • Uncert aint ies in global climat e sensit ivit y, due t o dif f erences in t he way physical processes and f eedbacks are simulat ed in dif f erent models • Uncert aint ies in regional climat e changes, which are apparent f rom t he dif f erences in regional est imat es of climat e

  7. How t o t ackle t he problem in assessment models ? I PCC Task Gr oup on Dat a and Scenar io Suppor t f or I mpact and Climat e Assessment (TGI CA) Gener al guidelines on t he use of scenar io dat a f or climat e impact and adapt at ion assessment - The I PCC Dat a Dist ribut ion Cent re (DDC) - Met hods of impact assessment

  8. How t o t ackle t he problem in assessment models ? • Dir ect using GCM simulat ion r esult in impact assessment � Keep model ’ s physical/ mat hemat ical consist ency � Pr ovide t r ansient simulat ion out put � Comput at ionally and r esour ce demanding � Pr ovide only one possible scenar io of t he f ut ur e t hat can not cover t he f ull r ange of t he uncer t aint ies • Nor malised Pat t er n Scaling met hod � Possibilit y t o r epr esent t he whole r ange of uncer t aint ies involved in f ut ur e climat e change pr oj ect ion � simple t o oper at e and comput at ionally f ast

  9. St eps of t he met hod 1. The st andar dised pat t er n of climat e change f r om t he GCM is est imat ed by dividing individual gr id box changes by t he global mean war ming of t hat model exper iment , yielding a r at io 2. The magnit ude of global war ming by a specif ied dat e in t he f ut ur e is est imat ed f r om t he simple model f or a given emissions scenar io and a given climat e sensit ivit y 3. The pat t er ns of changes in dif f er ent climat ic var iables ar e mult iplied by t he global war ming value f r om st age 2 � � � � � � � T ( T T ) / ( GMT GMT ) gcm gcm gcm gcm gcm ( 2070 / 2099 ) ( 1960 / 1990 ) ( 2070 / 2099 ) ( 1960 / 1990 ) � � � � � T T T GMT gcm ( 1 ) gcm ( 0 ) gcm sebm ( 1 )

  10. Weakness? A f undament al assumpt ion of t he scaling approach is t hat while t he magnit ude of climat e change alt ers over t ime in proport ion t o t he global warming, t he pat t ern of change f rom t he GCM remains const ant

  11. SimCLI M st ruct ure Greenhouse gas MAGI CC emission scenarios Dat a Global Climat e Proj ect ion Scenario select ions Climat e and GCM pat t ern import Local Climat e -Synt het ic changes t oolbox average, variabilit y, ext remes - GCM pat t erns (present and f ut ure) USER I PCC CMI P (GCMs) “ Plug-in ” Models Biophysical I mpact s on: - Land dat a Agricult ure, Coast al, - Ot her spat ial dat a Human Healt h, Wat er I mpact Model

  12. Advant ages of t he SimCLI M modelling approach • quick running and f lexible • spat ial and t emporal analyses • mult i-scale - nat ional, regional, sit es • Training – f or awareness raising • easily updat ed

  13. Mult i-scale, open-f ramework syst em

  14. Const r uct ing Climat e Change Scenar ios: spat ial Key uncer t aint ies: • Regional variat ions 1990 brings up baseline • Emission scenario climat e • Climat e sensit ivit y Scenario years up t o 2100 Climate feedbacks

  15. Const r uct ing Climat e Change Scenar ios: sit e specif ic

  16. SimCLI M can be used t o SimCLI M can be used t o • Describe baseline climat es • Describe baseline climat es • Examine current climat e variabilit y and • Examine current climat e variabilit y and ext remes ext remes • Assess risks – present and f ut ure • Assess risks – present and f ut ure • I nvest igat e adapt at ion – present and f ut ure • I nvest igat e adapt at ion – present and f ut ure • Creat e climat e change scenarios • Creat e climat e change scenarios • Conduct sensit ivit y analyses • Conduct sensit ivit y analyses • Examine • Examine sect oral sect oral impact s impact s • Examine uncert aint ies • Examine uncert aint ies • Facilit at e int egrat ed impact analyses • Facilit at e int egrat ed impact analyses

  17. Thank You! weiye@waikat o.ac.nz

Download Presentation
Download Policy: The content available on the website is offered to you 'AS IS' for your personal information and use only. It cannot be commercialized, licensed, or distributed on other websites without prior consent from the author. To download a presentation, simply click this link. If you encounter any difficulties during the download process, it's possible that the publisher has removed the file from their server.

Recommend


More recommend