Two solitudes - how seasonality biases drought from tree rings

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    Two solitudes - how seasonality biases drought from tree rings - Presentation Transcript

    1. TWO SOLITUDES how seasonality biases drought records from tree rings
    2. TWO SOLITUDES how seasonality biases drought records from tree rings
    3. why are Canadian streamflow reconstructions so lousy?
    4. 100% 80% 60% explained variance 40% 20% 0% Canada USA
    5. 100% Woodhouse et al., 2006 Meko et al., 2001 80% Sacramento River Upper Colorado River Meko et al., 2007 Colorado River Woodhouse, 2007 Middle Boulder Creek 60% explained variance 40% 20% 0% Canada USA
    6. 100% Woodhouse et al., 2006 Meko et al., 2001 80% Sacramento River Upper Colorado River Meko et al., 2007 Colorado River Woodhouse, 2007 Middle Boulder Creek 60% Case and MacDonald, 2003 explained Saskatchewan River Beriault and Sauchyn, 2006 Churchill River variance Bonin and Burn, 2005 Athabasca River 40% Watson and Luckman, 2005 Gedalof et al., 2007 Bow River Columbia River 20% 0% Canada USA
    7. why are Canadian tree rings not connected to climate modes?
    8. Janice Lough and Hal Fritts The Southern Oscillation and tree rings: 1600 - 1961 Journal of Applied Meteorology 24, 1985 Roseanne D’Arrigo and Gordon Jacoby A thousand year record of northwestern New Mexico winter precipitation reconstructed from tree rings and its relation to El Niño and the Southern Oscillation The Holocene 1, 1991 David Stahle and collaborators Experimental dendroclimatic reconstruction of the Southern Oscillation Stahle et al., 1998 Bulletin of the American Meteorological Society 79, 1998
    9. Prairie ringwidth records 138 Significant correlation with ENSO 4 Expected from random chance 6.9
    10. seasonality
    11. Trees, seasonality and climate forcings The southwestern US
    12. Trees, seasonality and climate forcings The Canadian Prairies
    13. DROUGHT AND SEASONALITY How does the connection between reconstructed drought 1 and seasonal precipitation vary across North America?
    14. DROUGHT AND SEASONALITY How does the connection between reconstructed drought 1 and seasonal precipitation vary across North America? CLIMATE MODES AND TREE RINGS In which regions are drought reconstructions most strongly 2 connected to remote climate forcings (ENSO, PDO, AMO)?
    15. The North American Drought Atlas Cook et al., 2007, Earth Science Reviews
    16. Cook et al., 2007, Earth Science Reviews
    17. CORRELATION COMPOSITES COHERENCE
    18. PART ONE tree rings, drought and seasonality
    19. significant (α=0.05)
    20. instrumental tree rings
    21. SUMM ER PRECIP ITAT ION
    22. WINTER PRECIPITAT ION
    23. do tree rings replicate these patterns?
    24. +
    25. summer mixed winter
    26. DOMINANT not exclusive
    27. “ ...the regional summer precipitation signal is strong in Pseudotsuga menziesii latewood-width [in southeastern Arizona]. David Meko and Chris Baisan Pilot study of latewood-width of conifers as an indicator of variability of summer rainfall in the North American monsoon region International Journal of Climatology 21, 2001
    28. Medicine Hat, Alberta Source: Environment Canada, Adjusted Historical Canadian Climate Data, 1895 – 2006
    29. Prairie ringwidth records 138 Significant correlation with ENSO 4 Expected from random chance 6.9 45
    30. ENSO and winter precipitation
    31. PART TWO drought records and climate modes
    32. ENSO PDSI from tree rings PDO AMO
    33. are these signals present in reconstructed drought?
    34. Julia Cole and Ed Cook The changing relationship between ENSO variability and moisture balance in the continental United States Geophysical Research Letters 25, 1998
    35. ENSO PDSI from tree rings PDO AMO
    36. COMPOSITES where is it wet or dry when ENSO is strong?
    37. ENSO PDSI from tree rings PDO AMO
    38. LOW frequency
    39. LOW FREQUENCIES (>7yr) TREE-RINGS and PDO 0.5 0.25 mean squared 61 0 coherence
    40. LOW FREQUENCIES (>7yr) TREE-RINGS and PDO 0.5 0.25 mean squared 61 0 coherence
    41. 3 Mexican PDSI 10 2 5 1 0 0 -1 -5 -2 -3 62 -10 1900 1920 1940 1960 1980 2000
    42. 3 PDO index Mexican PDSI 10 2 5 1 0 0 -1 -5 -2 -3 63 -10 1900 1920 1940 1960 1980 2000
    43. ENSO PDSI from tree rings PDO AMO
    44. SEAS ONALITY AND D ROUGHT
    45. summer mixed winter
    46. IMPLICATIONS 1590s
    47. IMPLICATIONS what/where OK
    48. IMPLICATIONS what/where OK what/where/why NOT OK
    49. IMPLICATIONS tree ring model output Celine Herwiejer, Richard Seager and Ed Cook North American droughts of the mid to late nineteenth century: a history, simulation and implication for Mediaeval drought The Holocene 16, 2006
    50. summer mixed winter
    51. M A N Y TH AN KS Dave Meko Ed Cook Hal Fritts Toby Ault

    + Scott St. GeorgeScott St. George, 2 years ago

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