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SECTION 4: RISK OVERVIEW <br />Climate change is expected to lead to an increase in average temperatures as well as an increase <br />in frequency, duration, and intensity of extreme heat events. With no reductions in emissions <br />worldwide, Texas is projected to experience an additional 30 to 60 days per year above 100°F <br />than what is experienced now.2 <br />The State Climatologist's Assessment of Historic and Future Trends of Extreme Weather in <br />Texas, 1900-2036 identifies ongoing and likely future trends out to the year 2036 based on <br />analysis of historic observations of temperatures, precipitation, and extreme weather. Table 4-4 <br />highlights future trends in extreme weather from the report. <br />Table 4-4. Future Trends in Extreme Weather in Texas3 <br />The average annual surface temperature in 2036 is expected <br />to be 3.0°F warmer than the 1950-1999 average and 1.8°F <br />warmer than the 1991-2020 average. <br />Nearly double the number of 100°F days by 2036 compared to <br />2001-2020. <br />Extreme Temperatures Higher frequency of 100°F days in urban areas. <br />Extreme monthly summertime temperature trends imply an <br />increase of about 1 OF compared to the 1950-1999 average. <br />Extreme monthly wintertime temperatures are expected to <br />continue to increase at an even faster rate. <br />The coolest days of the summer are expected to continue <br />becoming warmer. <br />Precipitation has increased by 10 percent or more in eastern <br />Texas, but little trend is present in western Texas. <br />Precipitation trends to 2036 are likely to be dominated by <br />natural variability. <br />Extreme precipitation is expected to increase in intensity on <br />Precipitation average statewide by 6-10 percent compared to the 1950- <br />1999 averages and 2-3 percent relative to the 2001-2020 <br />averages. <br />This translates to an increase in the frequency of extreme rain <br />of 30-50 percent relative to the climatological expected <br />frequency in 1950-1999 and 10-15 percent relative to 2001- <br />2020. <br />Increasing temperatures, rainfall variability, and other factors <br />will on balance decrease water availability, but impact <br />Drought changes will vary strongly across applications. <br />Impact trends to be highly sector -specific, with the impacts <br />possibly smaller for agriculture than for surface water supply. <br />2 U.S. Global Change Research Program, Washington, DC, USA, pp. 987-1035. doi: 10.7930/NCA4.2018.CH23. <br />https://nca20l8.globalchange.gov/chapter/23/ <br />3 Gammon -Nielsen, John, Holman, Sara, Buley, Austin and Jorgensen, Savannah. Assessment of Historic and Future <br />Trends of Extreme Weather in Texas, 1900-2036, 2021 Update. Texas A&M University Office of the Texas State <br />Climatologist. October 7, 2021. https://climatexas.tamu.edu/files/ClimateReport-1900to2O36-2021 Update <br />City of San Marcos I Hazard Mitigation Action Plan Update 2024 1 Page 6 <br />