Developing and Testing a Simple Approach for Projecting Temperature Trends to Facilitate Public Health Preparedness Público

Khargonekar, Shivangi Pramod (2012)

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Extreme heat events (EHEs) are expected to intensify in North America in the 21st
century, posing challenges outside current public health capacity. Adaptation will likely
be required to minimize health impacts. Most adaptation to date has been in response to
extreme weather events, e.g., the response to the European heat wave of 2003. The US
has not experienced a similarly dramatic EHE and likely has a significant preparedness
deficit. Scenario-driven table-top exercises are one way to facilitate preparedness, but
these require credible projections of climatic shifts. Downscaled projections are
computationally expensive, unavailable for most localities, and most public health
agencies cannot make their own. Given the advent of warming trends in many locales,
our objective is to determine whether it is appropriate to use historical weather data to
project future temperature trends. Such an approach is relatively straightforward,
intuitive, inexpensive, scalable, and generalizable compared with downscaled projections.
To test this proposition, we used a dataset of historical weather for selected major US
cities to identify appropriate indicators for projection, test multiple methods for
extrapolating historical trends, project findings forward by climate region and city, and
compare findings with available downscaled projections. Average daily temperature,
average daily maximum temperature, and maximum of the daily maximum temperature
in June-July-August (JJA) from 1950-2010 were selected as indicators. Stepwise
autoregressive methods were used to generate polynomial projections of the indicators.
The projections most consistent with historical data occurred with the indicators of
central tendency and showed mostly positive trends (e.g., average daily temperatures in
JJA in the Southeast are projected to increase by 5.6°F by 2035, and 10.0°F by 2055).
Negative trends for extremes (maximum of the daily maximum temperature in JJA)
resulted for three regions. The trends were determined to be a function of the
extrapolation method and greater variability in historical data for these regions. Available
downscaled regional projections were in concordance with our findings that much of the
US will experience warming in the future. We conclude that this approach has promise
but may systematically underestimate the magnitude of likely future temperature changes
in regions with variable historical temperature trends.

Table of Contents

Goals and Objectives.

Study Design.
Study Setting.
Site Selection.
Data Sources and Management
Data Analysis and Outcomes

Study Sample.
Variability of Historical Data
Comparisons with Downscaled GCM Outputs.

Variability of Historical Data
Study Strengths and Limitations

Tables and Figures.

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