decadal trends in extreme precipitation, winds, and snowpack over the northwest. cliff mass

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Decadal Trends in Extreme Precipitatio n, Winds, and Snowpack over the Northwest. Cliff Mass University of Washington

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Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass University of Washington. - PowerPoint PPT Presentation

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Page 1: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest.

Cliff Mass

University of Washington

Page 2: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

There has been a lot discussion in the media and in some of the

literature suggesting that western U.S. extreme

precipitation events have already increased in intensity or will

soon increase under anthropogenic global warming

Page 3: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass
Page 4: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Press AdvisoryNational Wildlife FederationNovember 17, 2009 Contacts:XXXX (name removed) YYYY (you know her!)Senior Environmental Policy Specialist Climate ScientistNational Wildlife Federation, Pacific Region National Wildlife Federation

… Global warming is exacerbating extremely heavy rainfall events, and recent climate change modeling suggests that these pineapple express storms are no exception. “Heavier rainfall events combined with significant snowmelt in midwinter is just what the Pacific Northwest should expect from global warming,” said Dr. YYYY, climate scientist, National Wildlife Federation.

…. Recent data[1] suggests that as a result of climate change, the largest storms (i.e., those that are most likely to cause flooding) will trend toward producing increasingly larger quantities of precipitation.

Page 5: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass
Page 6: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Others Have Suggested We Are Now Experiencing Extremes in Low

Northwest Snowpack and That Anthropogenic Warming is A

Significant Cause

Page 7: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

XXXXXXXXX

Page 8: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass
Page 9: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

And some have suggested that cold season storms, like our big

windstorms, will also get stronger

“There is also evidence of an increase in the intensity of storms in both the mid- and high-latitude areas of the Northern Hemisphere,”

State XState X

Page 10: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

This talk will suggest that some of these claims are inconsistent with

observations and the latest modeling results.

The truth is more complex and nuanced.

Page 11: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Our credibility is at stake

• Anthropogenic global warming IS a serious problem that must be dealt with.

• But by claiming excessive impacts on extremes we undermine our credibility and our ability to enhance society’s efforts to reduce greenhouse gas emissions and to precede with adaptation/mitigation.

Page 12: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Extreme Precipitation over the NW

There are several studies in the literature

Page 13: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Trends of 7-day extreme (1 yr or >): 1931-963 and 1-day extremes were similar

Little trend in the NW. Suggesting of small increases in western WA and decreases in western Oregon (tail indicates significant at 5% level)

Kunkel, Andsager, and Easterling, J. of Climate, 1999

Page 14: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

When it Rains it Pours (not reviewed) Used the Kunkel Approach for 1-day rainfall (1948-2006)

• More over Wa, LESS over Oregon, little trend, N. CA.

Page 15: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass
Page 16: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Are there trends in major precipitation

events?

• Examined top 20, 40, 60 two-day precipitation events at stations along the coast for 1950-2008.

Page 17: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass
Page 18: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Trends on Unregulated

Rivers1950-2009: Max Annual

Daily Discharge

Page 19: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Most modeling studies are inconclusive about whether global warming has influenced trends of extreme precipitation during the

past century.

Page 20: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

They ran contemporary dynamical downscaling (1970-2007):

• Hadley regional model forced by Hadley Center GCM• WRF forced by ECHAM5 GCM

Page 21: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

“The lack of correspondence between observed and simulated trends for extreme precipitation likely results from the dominance of natural variability over anthropogenic trends during the period 1970-2007.

Page 22: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Nearly are all heavy Northwest precipitation events are associated with the “Pineapple Express” (a.k.a.

atmospheric rivers) A relatively narrow current of warm, moist air from the

subtropics…often starting near or just north of Hawaii.

Page 23: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Atmospheric Rivers

• Atmospheric rivers are closely associated with the jet stream (on its southern side)

• Most General Circulation Models suggest the jet stream will move north and weaken under global warming.

• Thus, the atmospheric rivers may well move northward.

• Could our region thus experience a DECREASE in extreme precipitation?

Page 24: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Regional and Global Climate Simulations Indicate Substantial

Uncertainty for Extreme Precipitation over the Northwest

Under Global Warming

• Some even suggest a decline in winter precipitation

Page 25: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Simulated seasonal precipitation changes (mm/day) from 1989-1999 to 2045-2055 from the ECHAM5-MM5 regional model for a) DJF b) MAM c) JJA and d) SON

DJF

Page 26: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass
Page 27: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Other Research on Future Precipitation Trends over the NW:

No Agreement• Chen et al. (2003) examined the impacts of

doubling CO2 using MM5 and RegCM2 regional models to downscale the CCSM GCM simulation. – Found an increase in average precipitation over

central California and a decline over the Pacific Northwest.

Page 28: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Studies• Kim (2005) used the MAS regional model downscaled

from the HadCM2 GCM for 1990–2000 and 2040–49. Found the largest increases in extreme precipitation over northern California and Oregon, with little trend over Washington and southern California.

• Tebaldi et al. (2006) examined nine general circulation models found a general increase of extreme precipitation over the NW, with the magnitude of the positive trend increasing to the north, while decreasing or constant intensity was predicted over central and southern California.

Page 29: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Studies

• Duffy et al. (2006) used four regional climate models nested within two global ocean–atmosphere climate models, finding that the spatial distributions of precipitation vary substantially.

Page 30: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Extreme Precipitation Bottom Line

• The uncertainty of what will happen over the NW is huge.

• Simplistic talk about warming temperatures, causing more water vapor resulting in more extreme precipitation here should be avoided.

Page 31: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

West Coast Windstorms

• Increasing number of major windstorms from northern Oregon into southern BC

• Decreasing numbers to the south.

Page 32: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

West Coast Windstorms

• Northwest windstorms are closely associated with the strength and position of the jet stream.

• If the jet stream weakens and moves northward, what will happen to our winter storms?

• Will the decline in windstorms over the southern PNW move northward?

Page 33: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Snowpack Little Hint of Decline Due to

Anthropogenic Warming

Page 34: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

1950-2000

Page 35: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Washington-wide snowpack since 1950,Relative to 1971-2000 normal

Snowpack in usual maximum month

Page 36: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Washington-wide snowpack period of record,Relative to 1971-2000 normal

Snowpack in usual maximum month

Page 37: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass
Page 38: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

April 1 Snowpack

Page 39: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Remove Natural Variability

Slow steady decline over the past 80 years—no indication of anthropogenic global warming signal

Page 40: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

The NW is a location in which AGW temperature effects will be weaker

and delayed

1976-2007 temperature trends

Page 41: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Conclusions

• Changes in weather extremes over the Northwest have been highly heterogeneous, increasing some places and decreasing in others.

• Natural variability appears to be dominant.• There is no compelling evidence that

anthropogenic warming has had any influence on changes in Northwest weather extremes.

Page 42: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

Conclusions

• The future impact of anthropogenic global warming on NW extremes is highly uncertain.

• It may well be that extremes in precipitation and winds could decline over the NW under global warming.

• We must be very careful in communicating such uncertainties to our user communities.

Page 43: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

The End

Page 44: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass
Page 45: Decadal Trends in Extreme Precipitation, Winds, and Snowpack over the Northwest. Cliff Mass

60-year

Trendsfor

Top-60Events

IndividualStations

Two-degreebands