The Drying Climate in the American West

63rd Annual New Mexico Water Conference October 17, 2018 Las Cruces, NM

https://bit.ly/2NKGnsD

Lake Creek, Colorado Brad Udall September 8, 2018 Senior Scientist/Scholar Colorado State University [email protected]

Water Year 2018 Precipitation

Water Year 2018 Temperature Key Points

already impacting the basin – Temps for sure, maybe precipitation • Impacts will get Worse – “New Normal” inadequate to convey challenges – Aridification underway – not a • Plan on… – Heat! More and More as the Century Proceeds – Shifting runoff patterns • South (Dry) and North (Less Dry to Perhaps Wet) • Earlier within-year runoff – More WX Variability • year to year, within-year – Substantial Flow Reduction Risk – Substantial Megadrought Risk – Risks • Localized – Likely • Basin-wide - ?? – Higher Water Temperatures – • Opportunity for Change

The 2000-18 Millennium Drought is very, very different from previous in the historic record… Represents 6 maf loss over 18 years relative to worst 20th century drought Millennium Drought 2000—2018

• 2000-2017 is the worst drought in the gaged record • ~ 20%/yr decline • Long-term trend, too

Udall and Overpeck, WRR, 2017 Millennium Drought 2000—2018

• 2000-2017 is the worst drought in the gaged record • ~ 20%/yr decline • Long-term trend, too

• Lakes Powell and Mead have lost 50% of their volume

Udall and Overpeck, WRR, 2017 Millennium Drought 2000—2018

• Precipitation declines only partially explain • ~ 2/3 of the loss

Udall and Overpeck, WRR, 2017 Millennium Drought 2000—2018

• Precipitation declines only partially explain • ~ 2/3 of the loss

• Temperature increases explain the remainder • ~ 1/3 of the loss • Why? • More Evaporation • Thirstier Atmosphere

• Temperature-Induced Losses • Now = ~6% • 2050 = ~20% Udall and Overpeck, WRR, 2017 • 2100 = ~35% Udall and Overpeck, WRR, 2017 • Temperature can be a major flow driver • Since 1988 flows have been less than expected given winter precipitation • Warm temperatures exacerbated modest precipitation deficits in the Millennium Drought Model-based Study using Historical Data – Long-term Trend Analysis (-16.5% Decline) – Temperature De-trend Model Experiment – 1950s vs 2000s Drought Analysis – 2017 Forecast Analysis

• Findings – ~50% of Decline due to Higher Temperatures – ~50% of Decline due to Changing Precipitation Patterns 4 Key Basins (Green + Blue) produce ~55% of all runoff Denver Water Forecast Inflow vs Runoff 2018

• Colorado River snowpack peaked at 107% of normal

• South Platte River snowpack peaked at 85% of normal

April through July Natural Streamflow Percent of Average

South Platte at South Platte Blue River at Dillon Williams Fork Fraser at Winter Park

May 1 NRCS Forecast 48% 99% 81% 99% - Actual Natural Volume 38% 71% 71% 77% 22 %

Source: Denver Water Denver Water Forecast Inflow vs Runoff 2018

• Colorado River snowpack peaked at 107% of normal

• South Platte River snowpack peaked at 85% of normal

April through July Natural Streamflow Percent of Average

South Platte at South Platte Blue River at Dillon Williams Fork Fraser at Winter Park

May 1 NRCS Forecast 48% 99% 81% 99% -10% -28% -10% -22% Actual Natural Volume 38% 71% 71% 77%

Source: Denver Water New Normal?

It clearly will get hotter

Expansion of the Wet/Dry Axis = more variability

Hint of more occurrences of extreme wet than extreme dry

Note: precipitation is not runoff…

Dave Pierce, Scripps Aridification – not a drought

• Declining Snowpack and Aridity Index (P/PET) Changes earlier runoff • Higher Temperatures • Drying Soil • Thirsty Atmosphere • Moving tracks • Shorter Winter/Longer Fall • Greening ? • Megadrought?

Seager et al., 2018 Changing Precipitation Patterns: Dry South, Less Dry North

Changes in Soil Moisture in 2100

Climate models: north is wetter, and south is drier

Wet: Wind Rivers + Unita Mountains

Dry: Most of Colorado

Key: Where is the ‘hinge’ point? CRB Mainstem critical The Upper Colorado River Basin is Megadrought Country – 1200 years of Colorado River flow thanks to tree rings

Meko et al., (Geopysical Research Letters, 2007) Cook Science

In both Central Plains and Southwest, Multi- Percent Chance decadal Drought Risk* of Multi- st exceeds 80% in 21 Decadal Century Drought Risk, Southwest US * Defined as Drought lasting 35 or more years

P = +10%

P = +20% Risk = 70% w/ +10% Risk = 35% w/ +20% P = +10%

P = +20% Other Supporting Studies Snow Water Equivalent Trends

• Response of Colorado River runoff to dust in snow – Painter, et al., 2010 • Hydrologic Sensitivities of Colorado River Runoff to changes in Precipitation and Temperature – Vano et al., 2014 • Climatology, Variability, and Trends in the U.S. Vapor Pressure Deficit, an Important -Related Meteorological Quantity – Seager et al, 2015 • Running Dry: The US Southwest’s Shift to a drier climate – Prein et al., 2016

• Relative impacts of mitigation, temperature, and precipitation Mote et al., 2018 on 21st-century megadrought risk in the American Southwest – Ault et al., 2016 Vapor Pressure Deficit Trends • Evidence that Recent Warming is Reducing Upper Colorado River Flows – McCabe et al., 2017 • The Curious Case of Projected Twenty-First-Century Drying but Greening in the American West – Mankin et al., 2017 • Dramatic declines in snowpack in the western US – Mote et al., 2018 • The More Extreme Nature of North American Monsoon Precipitation in the Southwestern United States as Revealed by Seager et al., 2015 a Historical Climatology of Simulated Severe Weather Events – Luong, et al., 2018 Key Points

• Climate Change already impacting the basin – Temps for sure, maybe precipitation • Impacts will get Worse – “New Normal” inadequate to convey challenges – Aridification underway – not a drought • Plan on… – Heat! More and More as the Century Proceeds – Shifting runoff patterns • South (Dry) and North (Less Dry to Perhaps Wet) • Earlier within-year runoff – More WX Variability • year to year, within-year – Substantial Flow Reduction Risk – Substantial Megadrought Risk – Flood Risks • Localized – Likely • Basin-wide - ?? – Higher Water Temperatures – Fires • Opportunity for Change

Increasing Heat Content Everywhere

90% into the ocean FOLU = Forestry, Other Land Use Climate Change is Water Change

• Heat Drives the Water Cycle – 1000 km3 evaporates daily from the oceans

• The Water Cycle mixes heat from areas of too much to too little • As the Atmosphere Warms it Holds More Moisture: ~5F warming is 20% increase • Heating Up the Earth (and uneven heating) results in Water Cycle changes – More Evaporation, More Precipitation, More Moisture – Changes in weather patterns – Wet Wetter, Dry Drier Standard Rule – More Intense and Droughts • All Kinds of Water Changes Already Noted – More rain/less snow, Earlier Runoff, Higher Water Temps, More Intense Rain American Geophysical Union Fall Meeting – San Francisco

• December every Year • 24,000 Earth Scientists • Fully Accepted Science – Earth is Warming – Humans are the Cause – Very Risky to Burn Carbon unabated – Water Cycle will be Impacted • Theory vs “Belief” Almost every Major Scientific Organization has statement affirming Anthropogenic-caused Warming AND the need to act…

• National Academy of Science • All International Academies of Science • American Association for the Advancement of Science • American Geophysical Union • American Meteorological Society • The Geological Society of America • Many, many others..(but not AAPG) Climate Change Myths • Climate is always changing • It’s the sun • You said it was going to cool in the 1970s • Winter Related – It’s cold and snowy – We just set a cold record • Can’t predict weather, so can’t predict climate • Models are not any good… • 1930s were warmer... • It’s the Urban Heat Island Effect • It’s volcanoes Colorado River Future Flow Losses

Climate Change a combination of …

1. For-Sure Temperature Rise -> Flow Losses

2. Not-Sure Precipitation Change -> Flow Gains or Losses Evapotranspiration Increases in Natural Systems

Now Future

In the future, plants move up slope, increasing evapotranspiration.

By 2100 ET increases by 28% and Kings River flows decline by 26%. Colorado River Drought 2000-2014

• 2000-2014 Worst Drought in Colorado River Gage Record

• ~ 1/3 of the Decline due to Higher Temperatures

• 20% Loss by 2050 Possible due to higher temperatures

• Increases in precipitation may counteract losses somewhat

• Increased risk of megadrought in 21st century reinforces loss potential

Sources: Udall and Overpeck, 2017; Woodhouse et al., 2016