climate change

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By: kevdownes (22 month(s) ago)

I am a retired Head of Physics I am setting up a Module to encourage youngsters into engineering. I wonder if I may use it?

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Slide1:

Observed Changes to the Climate and their Causes By; gvm

Some human-induced environmental changes relevant to climate:

Some human-induced environmental changes relevant to climate Changes in land use (e.g. farming, building cities) Storage and use of water (dams, reservoirs, irrigation) Combustion of fossil fuels Generation of heat Generation of particulate pollution (e.g., soot, smoke) Generation of gaseous pollution  particulates (e.g., sulfur dioxide, nitrogen dioxide; get oxidized to form sulfate, nitrate) Generates carbon dioxide Generation of other greenhouse gases Methane, Nitrous oxide, Chlorofluorocarbons, Ozone  Especially via biomass burning, landfills, rice paddies agriculture, animal husbandry, fossil fuel use, leaky fuel lines, and industry  Changes the composition of the atmosphere   Most important are the gases with long lifetimes Like CO 2 > 100 years

Slide3:

The incoming energy from the sun is 342 W m -2 : but this is the 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 100 W = light bulb. So the energy from the sun is 120 million of these power stations. It shows: Direct human influences are tiny vs nature. 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

Slide4:

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

Slide5:

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!

Global Warming is happening:

Global Warming is happening Since 1970, rise in: Decrease in: Carbon Dioxide Snow extent Global temperatures Arctic sea ice Global SSTs Global sea level Tropical SSTs Water vapor Rainfall intensity Precipitation extratropics Hurricane intensity Drought

Slide7:

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

Slide8:

Heat Waves Impacts on human health and mortality, economic impacts, ecosystem and wildlife impacts

Slide9:

Extremes of temperature are changing! Observed trends (days) per decade for 1951 to 2003 From Alexander et al. (2006)

Slide10:

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

Slide11:

Global Sea Surface Temperature: base 1901-70 C

Slide12:

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

Slide13:

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

Slide14:

Water Holding Capacity 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. Observations show that this is happening at the surface and in lower atmosphere: This means more moisture available for storms.

Slide15:

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:

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Global warming  Heating   Temperature  & Evaporation   water holding capacity   atmospheric moisture    greenhouse effect  & rain intensity   Floods & Droughts

Slide17:

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).

Slide18:

Changes in hurricanes in the North Atlantic Ocean

Slide19:

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

Slide20:

Declines in sea ice and snow cover Runoff from earlier snow melt about 1-2 weeks earlier

Slide22:

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

Slide23:

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 SNOW PACK: In many land and mountain areas, global warming contributes to: Wildfire, near Denver CO: 2002

Slide24:

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

Slide25:

Palmer Drought Severity Index PDSI Dominant pattern: Upward trend. Dai et al 2004 Dry Wet

Slide26:

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

Slide27:

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.

Slide28:

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

Slide29:

CO 2 Temp.

Slide30:

Karl and Trenberth 2003

Natural forcings do not account for observed 20th century warming after 1970:

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

Climate change & other environmental issues are inter-linked:

Climate change & other environmental issues are inter-linked

Slide34:

World Population 6,640,000,000

Slide35:

Energy Food Water Biodiversity

Slide36:

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

Slide37:

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

Slide38:

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

Water Services:

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

Slide40:

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

Slide41:

The Challenge: Sustainable Management of an Ever-Changing Planet

Slide42:

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.

Slide43:

We need a better observing system! The challenge is to better determine the heat budget at the surface of the Earth on a continuing basis: Provides for changes in heat storage of oceans , glacier and ice sheet melt, changes in SSTs and associated changes in atmospheric circulation, some aspects of which should be predictable on decadal time scales.

Slide44:

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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