Global Warming: Coming ready or not!

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Transcription:

Global Warming: Coming ready or not! Help! Kevin E Trenberth NCAR

I wish to dedicate this lecture to Jim Hurrell Good health Jim!

The recent IPCC report has clearly stated that Warming of the climate system is unequivocal and it is very likely caused by human activities. Moreover, most of the observed changes are now simulated by climate models over the past 50 years adding confidence to future projections.

2007: The Nobel Peace Prize goes to the Intergovernmental Panel on Climate Change (IPCC) and Albert Arnold (Al) Gore Jr. "for their efforts to build up and disseminate greater knowledge about man-made climate change, and to lay the foundations for the measures that are needed to counteract such change".

2007 Coordinating Lead Authors NCAR Some Contributing Authors Lead Authors

1988 - The establishment of the IPCC Role of the IPCC: The role of the IPCC is to assess on a comprehensive, objective, open and transparent basis the scientific, technical and socioeconomic information relevant to understanding the scientific basis of risk of human-induced climate change, its potential impacts and options for adaptation and mitigation. Review by experts and governments is an essential part of the IPCC process.

1988 - The establishment of the IPCC WMO, UNEP 1990 - First IPCC Assessment Report 1992 - IPCC Supplementary Reports 1992- Adoption of the UNFCCC 1994- Entry into force of the UNFCCC Ratified by 189 countries 1994 - IPCC Special Report 1995 - Second IPCC Assessment Report 1996 - COP-2, 1997 - COP-3 1997- Adoption of Kyoto Protocol at COP-3 2005 Feb 16- Kyoto Protocol ratified by 164 countries (But not by USA or Australia) 2001 - Third IPCC Assessment Report 2002 - COP-8, 2003 - COP-9 2007 - Fourth IPCC Assessment Report

Scenarios of future emissions of greenhouse gases, aerosols Scenarios of future concentrations of greenhouse gases and aerosols Assessment of observations, processes and models Mitigation Policy options Adaptation Impacts Projections of future climate: The response, global, regional

A major strength of the IPCC process has been the intergovernmental process, through reviews and then approval of the Summary for Policy Makers on a word-by-word basis. This provides ownership. But it has also been subject to criticism as it is much more political. In principle, this process is designed to provide a report in which the content is determined by the science while how it is stated is determined jointly with the governments. Hence it aids communication between scientists and politicians. NOTE: In terms of impact of the report, the process is as important as the report itself.

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!

Changing atmospheric composition: CO 2 Mauna Loa, Hawaii Data from Climate Monitoring and Diagnostics Lab., NOAA. Data prior to 1974 from C. Keeling, Scripps Inst. Oceanogr.

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/

Key issue: What is your carbon footprint? Wgtn 4 Jul 07

The Natural Greenhouse Effect: clear sky O 3 8% Carbon Dioxide 26% CH 4 N 2 0 6% Water Vapor 60% Water Vapor Carbon Dioxide Ozone Methane, Nitrous Oxide Clouds also have a greenhouse effect Kiehl and Trenberth 1997

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

Global Warming is unequivocal Since 1970, rise in: Global surface temperatures Tropospheric temperatures Global SSTs, ocean Ts Global sea level Water vapor Rainfall intensity Precipitation extratropics Hurricane intensity Drought Extreme high temperatures Heat waves Decrease in: NH Snow extent Arctic sea ice Glaciers Cold temperatures

Global mean temperatures are rising faster with time Warmest 12 years: 1998,2005,2003,2002,2004,2006, 2001,1997,1995,1999,1990,2000 Period Rate 25 0.177±0.052 50 0.128±0.026 100 0.074±0.018 150 0.045±0.012 Years /decade IPCC

Land surface temperatures are rising faster than SSTs SST Land Annual anomalies of global average SST and land surface air temperature IPCC

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.

Air holds more water vapor at higher temperatures A basic physical law tells us that the water holding capacity of the atmosphere goes up at about 7% per degree Celsius increase in temperature. (4% per F) Observations show that this is happening at the surface and in lower atmosphere: 0.6 C since 1970 over global oceans and 4% more water vapor. This means more moisture available for storms and an enhanced greenhouse effect. Total water vapor IPCC

Land precipitation is changing significantly over broad areas Increases Decreases Smoothed annual anomalies for precipitation (%) over land from 1900 to 2005; other regions are dominated by variability. IPCC

Proportion of heavy rainfalls: increasing in most land areas Regions of disproportionate changes in heavy (95 th ) and very heavy (99 th ) precipitation IPCC

Declining Snow Pack in many mountain and continental areas contributes to drought moreprecipitation 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 soil moisture is less as summer arrives the risk of drought increases substantially in summer Along with wild fire

Drought is increasing most places Mainly decrease The most in rain over land important in tropics spatial and subtropics, pattern but enhanced (top) of by increased the atmospheric monthly demand Palmer with warming Drought Severity Index (PDSI) for 1900 to 2002. The time series (below) accounts for most of the trend in PDSI. IPCC

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.

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

Extremes of temperature are changing! Observed trends (days) per decade for 1951 to 2003: 5 th or 95 th percentiles From Alexander et al. (2006) IPCC

Heat waves are increasing: an example Extreme Heat Wave Summer 2003 Europe 30,000 deaths Trend plus variability? IPCC

Increases in rainfall and cloud counter warming Drought Trend in Warm Days 1951-2003 Absence of warming by day coincides with wetter and cloudier conditions IPCC

North Atlantic hurricanes have increased with SSTs (1944-2005) SST N. Atlantic hurricane record best after 1944 with aircraft surveillance. Marked increase after 1994 Global number and percentage of intense hurricanes is increasing IPCC

C Global SSTs are increasing: base period 1901-70

Sea level is rising: from ocean expansion and melting glaciers Since 1993 Global sea level has risen 43 mm (1.7 inches) 60% from expansion as ocean temperatures rise, 40% from melting glaciers Steve Nerem

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

Snow cover and Arctic sea ice are decreasing Arctic sea ice area decreased by 2.7% per decade (Summer: -7.4%/decade) 2007: 22% (10 6 km 2 ) lower than 2005 Spring snow cover shows 5% stepwise drop during 1980s IPCC

Surface melt on Greenland Increasing melt zones. Melt descending into a moulin: a vertical shaft carrying water to the base of the ice sheet. NSIDC (above) Braithwaite: Univ. Manchester

Karl and Trenberth 2003

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

Projected Patterns of Precipitation Change 2090-2100 Precipitation increases very likely in high latitudes Decreases likely in most subtropical land regions This continues the observed patterns in recent trends Summary for Policymakers IPCC

Arctic sea ice disappears in summer by 2050 Already 2007 lowest on record by 22% Abrupt Transitions in Summer Sea Ice 2007 x Gradual forcing results in abrupt Sept ice decrease Extent decreases from 80 to 20% coverage in 10 years. Relevant factors: Ice thinning Arctic heat transport Albedo feedback Holland et al., GRL, 2006

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

CO 2 Temp.

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

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. 175 countries have ratified Protocol was ratified; took effect Feb 16, 2005. US withdrew in 2001. In 2004 US emissions were 16% (20%) over 1990 levels for GHG (CO 2 ).

What about a carbon tax? Anyone can burn stuff and put Carbon Dioxide into the atmosphere as a waste product. If there was a value to Carbon Dioxide then this would presumably be reduced. A carbon tax, carbon emission limits, or pollution fines are designed to create a cost for burning carbon products, like coal and oil. Cap and Trade: Given a target (such as in the Kyoto Protocol) only so much can be burned and credits to allow burning can be traded (carbon emissions trading). Such a solution can be equitable if implemented across the board. But it can favor those who pollute if a country does not subscribe.

Recent trends: May 2007 Coal fired power stations have been brought on line at a rate of 2 per week over the past 5 years. China leads with one every 3 days or so (560 new plants from 2002 to 2006 and 113 GigaWatts of coal fired power). (200 MW each) Far from decreasing carbon dioxide emissions, the trend is much worse than business as usual and higher than A1FI. In 2030 global emissions will likely be up by 59% relative to 2004 according to the U.S. Energy Information Administration in its annual International Energy Outlook in May 2007. Raupach et al 2007 PNAS

The Kyoto Protocol basically calls for a freeze on emissions to 1990 levels for developed countries. Similarly, the Montreal Protocol for ozone depletion initially called for a freeze on CFC emissions and only later was this changed to a phase out. A freeze on emissions means that concentrations of carbon dioxide continue to increase. Climate continues to change, temperatures rise and sea level continues to rise.

We can slow global warming down! Disruption arises more from rapid change than from the climate per se. Mitigation effects mainly payoff beyond 2050. So we must adapt to climate change: we will adapt, whether unplanned (disruptive untold damage and loss of life), autonomously, or planned.

Many things you can do: Use energy efficient light bulbs Going Green!

Many things you can do: Walk, bicycle Drive less, and drive fuel efficient vehicles Use biofuels

Many things you can do: Do not over heat or over cool: Set thermostat to 76 F in summer Set to 66 F in winter Wear a sweater (82 F in Japan)

Many things you can do: Use solar power: Dry your clothes on the clothes line Some HOAs ban clothes lines: but clothes lines are environmentally beautiful

Many things you can do: Insulate your house etc:

Many things you can do: Use renewable energy Reduce coal fired power (unless carbon capture and storage employed)

Many things you can do: VOTE! Vote for responsible candidates Most important!

Our house Before After

The Challenge: Sustainable Management of an Ever-Changing Planet