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Global climate change and drought in the West Kevin E. Trenberth NCAR Global climate change and drought in the West Kevin E. Trenberth NCAR.

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Presentation on theme: "Global climate change and drought in the West Kevin E. Trenberth NCAR Global climate change and drought in the West Kevin E. Trenberth NCAR."— Presentation transcript:

1 Global climate change and drought in the West Kevin E. Trenberth NCAR Global climate change and drought in the West Kevin E. Trenberth NCAR

2 Climate The atmosphere is a “global commons.” Air over one place is typically half way round the world a week later, as shown by manned balloon flights. The atmosphere is a dumping ground for all nations for pollution of all sorts. Some lasts a long time and is shared with all. One consequence is global warming!

3 Data from Climate Monitoring and Diagnostics Lab., NOAA. Data prior to 1973 from C. Keeling, Scripps Inst. Oceanogr. Changing atmospheric composition: CO 2 Mauna Loa, Hawaii Changing atmospheric composition: CO 2 Mauna Loa, Hawaii

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5 CO2 emissions in different regions in 2000 in terms of emissions per capita (height of each block); population (width of each block); and total emissions (product of population and emissions per capita = area of block). Source: M. Grubb, http://www.eia.doe.gov/iea/

6 WaterVapor60% CarbonDioxide26% O 3 8% CH 4 N 2 0 6% 6% The Natural Greenhouse Effect: clear sky Clouds also have a greenhouse effect Kiehl and Trenberth 1997

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9 The incoming energy from the sun is 342 W m -2 : annual global mean: It amounts to 175 PetaWatts =175,000,000 billion Watts. About 120 PW is absorbed. The biggest power plants in existence are 1000 MegaWatts and we normally think of units of 1 KiloWatt (= 1 bar heater), or a 100 W light bulb. So the energy from the sun is 120 million of these power stations. It shows: 1)Direct human influences are tiny vs nature. 2)The main way human activities can affect climate is through interference with the natural flows of energy such as by changing the composition of the atmosphere

10 The enhanced greenhouse effect CO 2 has increased >33% If CO 2 were suddenly doubled then:  Atmosphere must warm up to restore balance via radiation to space  In absence of other changes: warming is 1.2°C  Feedbacks cause complications  Best estimate is warming of 2.9°C so feedbacks roughly double change  Real world changes complex and more gradual The enhanced greenhouse effect CO 2 has increased >33% If CO 2 were suddenly doubled then:  Atmosphere must warm up to restore balance via radiation to space  In absence of other changes: warming is 1.2°C  Feedbacks cause complications  Best estimate is warming of 2.9°C so feedbacks roughly double change  Real world changes complex and more gradual

11 Global Warming is happening Since 1970, rise in:Decrease in:  Carbon DioxideSnow extent  Global temperaturesArctic sea ice  Global SSTs  Global sea level  Tropical SSTs  Water vapor  Rainfall intensity  Precipitation extratropics  Hurricane intensity  Drought Since 1970, rise in:Decrease in:  Carbon DioxideSnow extent  Global temperaturesArctic sea ice  Global SSTs  Global sea level  Tropical SSTs  Water vapor  Rainfall intensity  Precipitation extratropics  Hurricane intensity  Drought

12 Variations of the Earth’s surface temperature Annual mean departures from the 1961-90 average for global temperatures, mean 14.0°C, and carbon dioxide concentrations from ice cores and Mauna Loa (1958 on), mean 333.7 ppmv. Updated from Karl and Trenberth 2003. Nonlinear fit Overall warming 0.75ºC Up 0.55ºC since 1970

13 Global SST: base period 1901-70 CC

14 Sea level is rising: from ocean expansion and melting glaciers Sea level is rising: from ocean expansion and melting glaciers Since 1993 Global sea level has risen 37 mm (1.46 inches) 60% from expansion as ocean temperatures rise, 40% from melting glaciers Steve Nerem Since 1993 Global sea level has risen 37 mm (1.46 inches) 60% from expansion as ocean temperatures rise, 40% from melting glaciers Steve Nerem

15 Impacts on human health and mortality, economic impacts, ecosystem and wildlife impacts Heat waves and wild fires

16 Europe summer temperatures Exceptional heat wave and drought of 2003 was a major extreme made more likely by global warming: 30K deaths From P. Jones

17 Water Holding Capacity A basic physical law tells us that the water holding capacity of the atmosphere goes up at about 4% per degree Fahrenheit increase in temperature. Observations show that this is happening at the surface and in lower atmosphere, by 4% since 1970 over global oceans. This means more moisture available for storms and an enhanced greenhouse effect.

18 Best estimate of linear trends for global ocean 1.3±0.3% per decade Sig. at >99% Trenberth et al. 2005 Best estimate of linear trends for global ocean 1.3±0.3% per decade Sig. at >99% Trenberth et al. 2005 Total column water vapor is increasing:

19 Changes in total, heavy, and very heavy precipitation over contiguous U.S. Linear trends are up and significant at 1%: 7, 14, 20% /century Groisman et al 2004 Changes in total, heavy, and very heavy precipitation over contiguous U.S. Linear trends are up and significant at 1%: 7, 14, 20% /century Groisman et al 2004 Changes in U.S. precipitation 1900 to 2002

20 Changes in hurricane frequency in the North Atlantic Ocean

21 Evidence for reality of climate change Glaciers melting 1900 2003 Alpine glacier, Austria 1900 2003 Alpine glacier, Austria 1858 1974 Grindelwald Glacier Switzerland 1858 1974 Grindelwald Glacier Switzerland 1909 Toboggan Glacier Alaska 2000

22 Evidence for reality of climate change Glaciers melting 1900 2003 Alpine glacier, Austria 1900 2003 Alpine glacier, Austria 1909 Toboggan Glacier Alaska 2000 Muir Glacier, Alaska

23 Declines in sea ice and snow cover

24 Recent warming greatest in the Arctic NSIDC, 2005

25 Precipitation Observed trends (%) per decade for 1951–2003 contribution to total annual from very wet days > 95th %ile. Alexander et al 2006 Regions where recent decades heavy precip >> mean precip updated from Groisman et al. (2005a).

26 Surface melt on Greenland Melt descending into a moulin: a vertical shaft carrying water to the base of the ice sheet. Braithwaite Univ. Manchester

27 Snow melt is occurring earlier along with runoff by 1 to 3 weeks. Larger circles indicate statistically significant trends at the 90% confidence level. From Stewart et al 2004 Climatic Change

28 more precipitation falls as rain rather than snow, especially in the fall and spring. snow melt occurs faster and sooner in the spring snow pack is therefore less as summer arrives soil moisture is less, and recycling is less global warming means more drying and heat stress the risk of drought increases substantially in summer along with heat waves and wildfires Wildfire near Denver 2002 SNOW PACK: In many mountain areas, global warming contributes to:

29 Human body: sweats Homes: Evaporative coolers (swamp coolers) Planet Earth: Evaporation (if moisture available) Human body: sweats Homes: Evaporative coolers (swamp coolers) Planet Earth: Evaporation (if moisture available) e.g., When sun comes out after showers, the first thing that happens is that the puddles dry up: before temperature increases. e.g., When sun comes out after showers, the first thing that happens is that the puddles dry up: before temperature increases.

30 Global warming  Heating   Temperature  & Evaporation   water holding capacity   Heating   Temperature  & Evaporation   water holding capacity 

31 Drought: 3 kinds of drought 1.Meteorological: absence of rain 2.Agricultural: absence of soil moisture 3.Hydrological: absence of water in rivers, lakes and reservoirs Drought: 3 kinds of drought 1.Meteorological: absence of rain 2.Agricultural: absence of soil moisture 3.Hydrological: absence of water in rivers, lakes and reservoirs

32 Lake Dillon, Colorado, August 8, 2002 Courtesy R. Anthes Lake Dillon, Colorado, August 8, 2002 Courtesy R. Anthes

33 © Ron Niebrugge The New York Times MAY 2, 2004 Drought Settles In, Lake Shrinks and West's Worries Grow PAGE, Ariz. - At five years and counting, the drought that has parched much of the West is getting much harder to shrug off as a blip. Some of the biggest water worries are focused here on Lake Powell... © Ron Niebrugge

34 The Colorado River Basin is now in its 5th year of drought. Inflow volumes have been below average for 4 consecutive years, with 2004 now certain to follow suit. Low inflows the past 5 years have reduced water storage in Lake Powell. The current elevation (as of September 22, 2004) of Lake Powell is 3,571 feet (129 feet from full pool). Current storage is 9.2 million acre-feet (38% of live capacity). http://www.usbr.gov/uc/water/crsp/crsp_cs_gcd.html Lake Powell has not been this low since 1970 As of September 22, 2004: 38% of capacity minimum level for power generation = 3490 ft Filling Since 1963 R Seager

35 Lake Powell Elevation Through July 26, 2006 Min 2005 0408 3555.1’ -144.9’ July 26, 2006: -92’, 3607.7’ www.usbr.gov/uc/water/index.html Inflows since 2000: est 73 % Now –2.0 inches per day FILLING UP

36 60 yr smoothed reconstruction Western US Cook et al Science Nov 2004

37 % US west of the Rocky Mountains dry (top) or wet (bottom) based on PDSI for moderate to extreme drought or wet. From NOAA NCDC.

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39 Rising greenhouse gases are causing climate change, and arid areas are becoming drier while wet areas are becoming wetter. Water management:- dealing with how to save in times of excess for times of drought – will be a major challenge in the future. Rising greenhouse gases are causing climate change, and arid areas are becoming drier while wet areas are becoming wetter. Water management:- dealing with how to save in times of excess for times of drought – will be a major challenge in the future.

40 Palmer Drought Severity Index PDSI first EOF: trend. 6.7% variance Dai et al 2004 Palmer Drought Severity Index PDSI first EOF: trend. 6.7% variance Dai et al 2004

41 Wet Dry Dry: PDSI +3.0 % Dry and Wet Areas over Global Land Increasing separation due to increasing temperatures and demand of atmosphere for more moisture

42 Karl and Trenberth 2003

43 Natural forcings do not account for observed 20 th century warming after 1970 Meehl et al, 2004: J. Climate.

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45 Source: Hansen, Climatic Change 2005, based on Petit, Nature 1999 Context: 400,000 years of Antarctic ice core records of Temperatures, Carbon dioxide and Methane. Last ice age glacial: 20,000 years ago

46 CO 2 Temp.

47 Climate change & other environmental issues are inter-linked

48 Food and Fiber Production Provision of Clean and Sufficient Water Maintenance of Biodiversity Maintenance of Human Health Storage and cycling of Carbon, Nitrogen, Phosphorus Agricultural Lands Coastal Zones Forest Lands Freshwater Systems Arid Lands Grasslands Climate change will affect the ability of ecological systems to provide essential ecological goods and services

49 Food production needs to double to meet the needs of an additional 3 billion people in the next 30 years Climate change is projected to decrease agricultural productivity in the tropics and sub-tropics

50 Wood fuel is the only source of fuel for one third of the world’s population Wood demand will double in next 50 years Climate change is projected to increase forest productivity, but forest management will become more difficult, due to an increase in pests and fires

51 Water Services One third of the world’s population is now subject to water scarcity The population facing water scarcity will more than double over the next 30 years Climate change is projected to decrease water availability in many arid and semi-arid regions

52 Climate change will exacerbate the loss of biodiversity Estimated 10-15% of the world’s species could become extinct over the next 30 years Biodiversity underlies all ecological goods and services

53 The Challenge: Sustainable Management of an Ever-Changing Planet

54 The UN Framework Convention on Climate Change Ratified by 189 countries Ratified by the US Article 2 is statement of the objective Convention entered into force 21 March 1994

55 Background -- Kyoto Protocol A legal instrument under UNFCCC Requires net reduction in developed country averaged annual GHG emissions of 5% (US 7%) over the period 2008-12 compared to 1990 levels “Basket” of ghgs (CO 2, CH 4, N 2 O, HFCs, PFCs, SF 6 ) Provisions for “flexible” market mechanisms: international trading system, credits, etc. 164 countries have ratified Protocol has now been ratified; took effect Feb 16, 2005. US withdrew in 2001. In 2004 US emissions were 16% (20%) over 1990 levels for GHG (CO 2 ).

56 Global warming actions There are uncertainties about how climate will change. But climate will change. And it could be very disruptive. There will be substantial costs incurred; -often by innocent people and countries Global warming actions There are uncertainties about how climate will change. But climate will change. And it could be very disruptive. There will be substantial costs incurred; -often by innocent people and countries The issue is directly linked to  fossil fuel energy use.  security (foreign oil imports).  sustainability. Oil supplies will be exceeded by demand sooner or later and long before we run out. The issue is directly linked to  fossil fuel energy use.  security (foreign oil imports).  sustainability. Oil supplies will be exceeded by demand sooner or later and long before we run out.

57 The parable of the frog A frog placed in a pot of hot water, immediately jumps out to save himself. But a frog placed in a pot of cold water that is slowly brought to the boil, remains in the pot and dies! Is this a parable for global warming?


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