Adel Hanna 1, Jason Ching 1, Joseph Pinto 2 1 UNC Institute for the Environment, Chapel Hill, NC, USA 2 National Center for Environmental.

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Presentation transcript:

Adel Hanna 1, Jason Ching 1, Joseph Pinto 2 1 UNC Institute for the Environment, Chapel Hill, NC, USA 2 National Center for Environmental Assessment, US Environmental Protection Agency, RTP, NC, USA Characteristics of Heat Wave Impacts for Major Cities in the US under Current and Future Climate Conditions

Outline Motivation and Objectives Heat Waves o Impacts, Metrics and Indices Climate Scenarios o Downscaling approach - WRF and CCSM Wet Bulb Globe Temperature (WBGT) Local Climate Zones (LCZs) Utilize LCZ to drive WBGT urban texture within mesoscale model grids cells Demonstrate WBGT variability for Chicago and Atlanta for different climate scenarios Summary of Findings Future Directions and Conclusions

Major global concern regarding the increased frequency and severity of heat waves and their impacts.

Objectives  Provide a modeling platform for bridging the gap between the operational mesoscale modeling and neighborhood scale modeling for characterizing heat stress in two major cities in the US  Integrate highly computational information based on downscaling global climate models to regional models with urban texture parameters mapped based on parameters and their values from Local Climate Zones (LCZs) (Stewart and Oke, 2012)  Compute and analyze heat stress risk levels based on the wet bulb globe temperature(WBGT) under current and future climate conditions  Examine the effect of intra-urban differences on heat stress based on the use of LCZs  Develop recommendations incorporating WUDAPT with operational regional scale modeling for heat stress advisories

Heat Waves Impacts o Health, economics, loss of labor hours Introduction of the WBGT as an index for assessing the health impact of heat waves on mortality, morbidity, and comfort. Impact of the occurance and frequency of extreme values of WBGT and its variability geographically and climate changs Why Wet Bulb Globe Temperature (WBGT) o A metric that considers dry bulb temperature, wet bulb, and globe temperature o The globe temperature is a temperature from a black globe thermometer measuring solar and other ambient radiation to represent the temperature at which heat transfer from the human body is equal to the radiant heat transfer in the actual non-uniform enclosure. o Only metric to have defined thresholds

Wet Bulb Global Temperature, WBGT ( See Kusaka et al.,(2012)) WBGT= 0.7WBT + 0.1T d T Globe T Globe = T d S U WBTWet Bulb Temperature T d Dry Bulb Temperature T globe Globe temperature SIncoming solar radiation UWind speed Applications and correspondence to risk assessment o Developed to help control heat causalities during military training o Correlates better than air temperature to the number of heat strokes patients

WRF model domains Model Years (2003, 2050) o Dynamical downscaling of the CCSM meteorological outputs to provide initial and boundary conditions at 108 km grid resolution for WRF nested at km grid resolutions o SRES A1B driven CCSM results used for IPCC AR4 on a T85 Gaussian grid. o May, June, July, and August of the years 2003, representing current climate conditions; and the year 2050, representing future climate conditions. o WRF Model hourly outputs at 12km x 12km over USA, can be finer (4km x 4 km) or at even higher resolutions for more refined urban simulations. Climate Scenarios

CCSM (108km) Monthly average for August Note the expansion of the Bermuda High westward and northward (e.g., 1020mb contours & broadening and strengthening of the warm sectors)

Local Climate Zones (LCZ) (as rendered by the WUDAPT Project) Table lookup Parameters Sky View Factor Building heights Roughness Radiative properties Etc Each city has its distinctive spatial patterns and distributions of LCZ

WBGT ( o C) Heat Stress Risk Levels (Kusaka et al., 2012) WBGT < Atlanta WBGT < Chicago Number of hours corresponding to WBGT Range

Cumulative Distribution of WBGT Warming trend in 2050 for both cities is clear The impact on Chicago (in terms of WBGT differences) seem to be larger than Atlanta

WBGT Time Series  General warming trend for year 2050  Atlanta shows higher number than Chicago of heat stress related health impacts

Box Plots Overall increase across the distribution for both cities from 2003 to 2050 Median

Model sensitivity to grid size & ability to resolving details of underlying surfaces 12 km grids 36 km grids The finer the grid mesh, the better to resolve the details of the underlying surfaces, the more appropriate is the model physics applicable to the dominant land features LCZ classes For Chicago

Urban variation in WBGT sensitivity to its Sky View Factor, SVF Sky View Factor (SVF) Sensitivity of WBGT in terms of its effect on solar radiation on T Globe WBGT= 0.7WBT+0.1T d +0.2 T Globe T Globe = T d S wrf U Replacing S wrf with S urban Where S urban = S wrf x SVF (Kusaka et al., 2012) SVF = 0 Sky view completely obstructed SVF = 1 Sky view completely unobstructed (WRF) and U = output of regional model, WRF, or U = 1 msec -1 (for illustration purposes)

Sensitivity of WBGT to Sky View Factor (SVF) actoractor Differences of more than 3.0 are seen particularly during June and July 1/3 the range of concern of heat stress risk levels Significant diurnal variability in WBGT

Summary and Findings  This Pilot Study was performed; designed to explore the operational feasibility of providing heat stress indices (WBGT) and advisories based on current and mid century climate prediction scenarios for two cities, Chicago and Atlanta Utilized offline outputs of WRF model based on downscaling CCSM under current (Year 2003) and future (Year 2050) climate conditions as input to calculate WBGT time series (May to Aug) Results show higher heat stress in 2050 simulations for both cities Synoptic responses between the base and future year for each city differed during the 4 month period Significant diurnal variation in WBGT and significant range of intra-urban (as subgrid) variability due to the potential range of LCZs (represented by SVF in this case) present in coarse operational grid systems.

Future Directions and Conclusions The output of regional modeling results can be used to calculate WBGT on an operational bases Intra-urban variations in WBGT may be introduced through the utilization of Table Lookup values of parameters of LCZs (especially SVF) superimposed as spatial weighting maps. Conceptually, the extension of this effort could be extended to provide advisories anywhere in the world. We envision this by the incorporation of WUDAPT Level “0” Census of Cities data. WUDAPT would provide on a worldwide bases. LCZ and the relevant parameters of the intra-urban heat stress advisories for all major cities in the world Provisions (through the URBPARM table in WPS/WRF) for urban options to run WRF anywhere in the world, on an operational bases. Further efforts will be required to test and evaluate the feasibility of these suggestions.

Acknowledgments EPA- STAR program R Disclaimer: The views expressed are those of the authors and do not necessarily represent views or policies of the U.S. Environmental Protection Agency

Thank You