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Climate Modeling for the Asia-Pacific

CIFOR-ICRAF
Mar. 1, 2016
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Climate Modeling for the Asia-Pacific

  1. Climate Modeling for the Asia-Pacific -- ClimateAP and its applications Tongli Wang, PhD Faculty of Forestry University of British Columbia
  2. Change in global temperature 2 IPCC fifth report
  3. Historical change in CO2 level and temperature 3Source: http://www.brighton73.freeserve.co.uk/gw/paleo/400000yearslarge.gif
  4. C02 emission scenarios 4
  5. Projected future climates (IPCC AR5) 5
  6. Forests and climate change • Climate change mitigation • CO2 Sequestration • Green materials – to reduce the use of CO2 emission intensive materials • Adaptation to climate change • To serve as a sink not a source of CO2 6 Carbon sink Carbon source
  7. Effects of climate on forest trees • Climate is a major environmental factor affecting the performance of trees (environmental effect) • Climate is also the most important evolutionary force causing speciation and within-species variation (genetic effect) in plants 7
  8. Globally, forest types are associated with climate types
  9. Regionally, each tree species is adapted to a range of climatic conditions - climatic niche
  10. Climate also shapes among-population variation along climate gradients within a species Species range of lodgepole pine Climatic niche Productivity
  11. Climate change causes mismatches between the climate that trees adapted and the climate that trees are going to experience 11 Productivity Current Future
  12. Some existing trees will move out their suitable climate habitat Waste of natural resources 12
  13. Current climatic niche distribution Future climatic niche distribution Lagging edge population extirpation Adaptation over generations using standing variation and gene flow Natural migration from leading edge Natural population responses Climaticgradient warm cold Aitken et al. 2015
  14. A framework for climate change adaptation in forestry 14 • Climate data for the past and the future Climate data Impact assessment Adaptation strategies • Plant-climate relationships • Projections on tree species ranges • Climate-based forest resources management • Knowledge transfer (web tools)
  15. Challenges in getting climate data • Not easy to access for specific locations • Not at a desirable resolution • Not at an expected accuracy • Not having enough biological relevant climate variables • Historical and future from different sources • Different resolutions and variables 15
  16. Climate Modeling – Climate AP Interface Coverage
  17. How does it work? • 1. Data sources • 2. Downscaling algorisms • 3. Calculated and derived climate variables • 4. Integrations and downscaling of historical and future climate data • 5. A user-friendly interface
  18. 1. Data sources ClimateAP • Baseline data (1961-1990 normals) • PRISM data at 4km for China • WorldClim (4km) for the rest • Historical annual data • CRU: 1901 – 201x • Future projections • GCM projections from IPCC AR5 18
  19. 2. Downscaling of the baseline data • A combination of • bilinear interpolation and • Elevation adjustment bilinear interpolation Elevation adjustment
  20. Approaches for elevation adjustment • Polynomial functions 𝑦 = 𝑎 + 𝑏1𝑥1 + 𝑏2𝑥2 + ⋯ + 𝑐1𝑥12 + 𝑐2𝑥22 + ⋯ • Partial derivative functions based on PRISM data that incorporated topography and expert knowledge • Dynamic local regression elev MAT   = – 0.0183 + 5.5910–4  Lat – 2.2910–6  Lat  Long )( PRISMsite elev MAT elevelev   
  21. Dynamic local elevational adjustment 21 Calculate differences between each of the 36 unique pairs
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  24. Improvements by ClimateAP 25 Fujian pilot site
  25. ClimateBC is critical for climatic mapping BEC zones Observed Predicted Source: Hamann & Wang. 2005. Models of climate normals for genecology and climate change studies in BC. Agricultural and Forest Meteorology 128: 211-221
  26. 3. Calculated and derived climate variables • Calculate climate variables • Temperatures: MAT, MWMT, MCMT, TD, • Precipitation: MAP and MSP • Dryness: AHM and SHM • Radiation: MAR • Derived climate variables • Degree-days: DD<0°C, DD>5°C, DD<18°C and DD>18°C • Frost: NFFD, FFP, bFFP, eFFP • Dryness: Eref and CMD • Snow: PAS Weather stations
  27. 4. Integrations and downscaling of historical and future climate data 29
  28. GCM data for future climate Resolution at 3.75 x 3.75° 30GCM data (CanESM2 RCP4.5 2050s)
  29. Downscaling approach Future climate data GCM Anomaly Reference period 1961-1990 Replaced by ClimateAP Interpolation ClimateAP output +
  30. It facilitates predictions for management unit 32 Current Future (2050s) Climate Ecosystems UBC Research Forest
  31. ClimateAP output is better than original GCM or RCM Tmax07 of 2011
  32. ClimateAP generates climate data for the past years (1901 – 2012) 3434
  33. ClimateAP includes 19 GCMs and 41 CC scenarios for three future periods 3535
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  38. ClimateWNA has been Widely used for climate related studies 40 0 200 400 600 800 1000 1200 Number of citations Year This will likely to be the future for ClimateAP! ClimateWNA
  39. Future development: adding future annual data to ClimateAP • To reflect annual variability and extremes • 2 scenarios, 3 GCMs and 90 years = 540 sets • Programming to achieve fast access to the time series data
  40. A framework for climate change adaptation in forestry 42 • Climate data for the past and the future Climate data Impact assessment Adaptation strategies • Plant-climate relationships • Projections on tree species ranges • Climate-based forest resources management • Knowledge transfer (web tools)
  41. Conditions for ecological niche models
  42. Modeling and projecting bioclimate envelopes for BC ecosystems and tree species • The basis: • The relationship between the realized niche and climate variables • Assumption: • The realized niche is the result of local adaptation and interactions with other species and organisms under recent/historical climatic conditions • Major challenges • Model accuracy • Uncertainty associated with uncertain future climates 44
  43. Predicting BC ecosystem Climate data Ecosystem classifications 45
  44. Improvement in model accuracy • PCA • Discriminant analysis • Machine-learning methods • Neural network • Random Forest + • Optimizations 46
  45. Observed vs. predicted BC ecosystems 47 BEC Zones (observed) BEC Zones (predicted)
  46. A local application: predictions of Subzones 48Kamloops Timber Supply Area (at 90m) Predicted (current) Mapped
  47. We chose 20 scenarios to represent the range and distribution Predicted changes in temp. and precip. for BC by 134 climate changes scenarios for 2050s 49
  48. Projected ecological responses to six selected climate change scenarios for 2050s A consensus projection for 2050s 50
  49. Consensus predictions among the 20 selected climate change scenarios 51
  50. Model-agreement among the projections based the 20 selected climate change scenarios 52 (Wang et al. 2012)
  51. Results adapted into forestry policy
  52. Climate niche Models – Chinese fir • Contraction is the substantial • Expansion is limited • Concerned! Wang et al. 2016
  53. Masson pine Wang et al. 2016
  54. Chinese pine Wang et al. 2016
  55. Blue gum Wang et al. 2016
  56. Google map based ClimateAP (http://climateap.net/ ) • Spatial visualization • Data access Web-based climate tools for APFNet Output 6 This web tool makes the spatial visualization easy and simple, and delivers the output data to users’ figure tips through a web browser.
  57. Future development: more species and ecosystems • More species: 10 species • China: two larch (Larix gmelinii and L. olgensis) species, Scots pine (Pinus sylvestris), Yunnan Pine (Pinus yunnanensis), black locust (Robinia pseudoacacia), Chinese cork oak (Quercus variabilis), aspen (Populus tremula), moso bamboo (Phyllostachys edulis) • Chinese Taipei: Cyclobalanopsis longinux (syn. Quercus longinux), Lithocarpus megalophyllus (?)
  58. Available ecosystem classifications
  59. Climatic modeling for ecosystems Current Future Wang et al. 2012
  60. CC Impacts differ among ecological zones Sub-Boreal Spruce zone Interior Cedar- Hemlock zone Current CGCM3 A2 2080s Contraction Expansion 62 Wang et al. 2012
  61. Associate tree species with ecosystems 63 Douglas-fir Associate Project Future
  62. Conclusions • ClimateAP • uses of the best available climate data and improves them • Adds a large number of climate variables • Offers a n all-in-one package: historical, current and future • User friendly interface • It facilitates ecological modelling at both species level to study the trend and local management unit to develop adaptive management strategies • Our climatic and ecological models are competitive and accessible at your figure tips.
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