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UK-US Workshop Part V: Broadening the portfolio of climate information

by Judith Curry

This post discusses Workshop presentations on broadening the portfolio of climate information for use in regional adaptation decisions.

This post is a follow-on to the four previous posts:

Projections of future climate variability and change on decadal (nominally 10-40 years from now) and regional scales are of high relevance for decision making.  However, these time and space scales are  particularly challenging for climate models because natural variability can be at least as large as forced climate variability.

Broadening the portfolio of climate information used to support decision making is envisioned to integrate the following elements:

This post highlights two presentations that relate to broadening the portfolio of climate information to support decision making:

Rob Wilby – Climate ‘hot spot’ analysis to inform adaptation planning in Yemen

Development agencies can face difficult decisions about where and how to prioritise investments in climate risk reduction measures. Community level adaptation options in semi-arid regions include rainwater harvesting, terrace rehabilitation, re-afforestation, wadi bank protection, irrigation schemes, small dams, training village-level agriculture technicians (extension workers/ veterinarians), establishment of saving and credit groups and provision of small grants for income generating activities, and literacy training. Implementation is especially challenging in data sparse regions where there may be few meteorological stations, complex topography and extreme weather phenomena.  This paper describes the development and application of a decision-support tool to identify ‘hot spots’ of climate risk and to guide adaptation activities in Yemen. The project was commissioned by the United Nations International Fund for Agricultural Development (IFAD) in order to identify ~500 village units that are vulnerable to flash flooding, soil erosion, water scarcity and reduced crop potential. We blended surface meteorological observations, remotely sensed (TRMM and NDVI) data, physiographic indices, and regression techniques to produce gridded maps of annual mean precipitation and temperature, as well as parameters for site-specific, daily weather generation for any location in Yemen. Climate sensitivity analysis was then applied to the impact models alongside socio-economic criteria to identify communities that are potentially most at risk. Finally, a Google Earth tool was provided to enable field officers to locate communities and interpret climate risks within a wider landscape context.

Judith Curry – Generating possibility distributions of scenarios for regional climate change

At timescales beyond a season, available ensembles of climate models do not provide the basis for probabilistic predictions of regional climate change.  Given the uncertainties, the best that can be hoped for is scenarios  of future change that bound the actual change, with some sense of the likelihood of the individual scenarios.  This talk argues that this is a realistic expectation for timescales out to 2040 or 2050.

Scenario thinking – Scenarios are provocative and plausible accounts of how the future might unfold. The purpose is not to identify the most likely future, but to create a map of uncertainty of the forces driving us toward the unknown future.  Scenarios help decision makers order and frame their thinking about the long-term while providing them with the tools and confidence to take action in the short-term.

Are GCMs the best tool? – GCMs may not be the best tool, and are certainly not the only tool, for generating scenarios of future regional climate change.  Current GCMs inadequate for simulating natural internal variability on multidecadal time scales.  Computational expense precludes adequate ensemble size.  GCMs currently have little skill in simulating regional climate variations.  Dynamical & statistical downscaling adds little value, beyond accounting for local effects on surface variables.  Further, the CMIP5 simulations only explore various scenarios of emissions, they do not explore multiple scenarios of solar forcing.

Possibility theory provides a useful framework for considering scenarios.  Possibility theory is an imprecise probability theory that states that any hypothesis not known to be impossible cannot be ruled out. A possibility distribution distinguishes what is plausible versus the normal course of things versus surprising versus impossible.

The challenge for identifying an upper bound for future scenarios is to identify the possible and plausible worst case scenarios.   What scenarios would be genuinely catastrophic? What are possible/plausible time scales for the scenarios? Can we ‘falsify’ these scenarios for the timescale of interest based upon our background knowledge of natural plus anthropogenic climate change?

On decadal timescales, the scenarios of greatest interest involve extreme weather events.  The decadal scenarios are not time series, but rather frequencies of extreme events (including clusters) and worst case scenarios over the target time interval:  floods, droughts, heat waves, tropical cyclones, heavy snowfalls, etc.

Data driven scenario generation methods:
  • Climatology (historical, paleoclimate)
  • Extrapolation of recent trend
  • Dynamic climatology empirical model  (Suckling/Smith)
  • Network-based dynamic climatology (Wyatt & Curry)
  • Secular global warming as a multiplier effect
  • “What if” scenarios relative to vulnerability threshold
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Scenarios (insights) for 2015-2025
Stadium wave climate dynamics:
  • Warm AMO (shifting towards neg), cool PDO
  • More La Nina events
  • Decrease/flattening of the warming trend

Weather/climate impacts for U.S. (analogue: 1955-1965):

  • more rainfall in NW, mid Atlantic states
  • less rainfall in W/SW, Texas
  • more hurricane landfalls along Atlantic coast, fewer in FL

“Spiking” from AGW:

  • Increasing rainfall
  • Increase in hurricane intensity
  • Overall reduced hurricane landfall owing to eastward extension of the Atlantic warm pool

Scenarios (quantitative guidance) 2015-2025

Methodology for scenario generation using stadium wave dynamics:
  • Generate a large synthetic climatology of the event using Monte Carlo resampling from the pdfs conditioned on the particular regime.
  • Utilize extreme value theory to extrapolate the historical data into a far tail region so as to be able to simulate more extremes.
  • Identification of ‘clustering’ of events, both intraseasonal and over periods of 3 years or less. Extreme events can arise from a single extreme storm, a correlated series of smaller events, or from antecedent conditions

Likelihoods for the possibility distributioncan be developed by:

  • Weighting preference for scenario generation method
  • Historical precedent
  • Expert judgment
  • Number of independent paths for reaching a particular scenario event

Conclusions

GCMs are not the only, or best, way to generate future scenarios of regional climate change

On decadal time scales, the greatest vulnerability is to extreme weather events:  scenarios of frequency (clustering), worst case

Climate science in support of developing empirical approaches for scenario development:

  • Improved regional historical and paleo records of extreme events
  • Improved statistical methods for analyzing extreme events
  • Improved understanding of the climate dynamics of extreme events and natural variability of regional climate
  • Scenario discovering using a broader range of approaches
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