GLOBAL WARMINGPREPARED BY

Ömer Veli Yeşilyurt

Global warming is the increase in the average measured temperature of the Earth's near-surface air and oceans since the mid-20th century, and its projected continuation.

The average global air temperature near the Earth's surface increased 0.74 ± 0.18 °C (1.33 ± 0.32 °F) during the 100 years ending in 2005.

Global warming is a result of increasing concentrations of atmospheric aerosols that block sunlight from reaching the surface, has partially countered the effects of warming induced by greenhouse gases.

Global Warming

Source: Intergovernmental Panel on Climate Change

According to the National Academy of Sciences, the Earth's surface temperature has risen by about 1 degree Fahrenheit in the past century, with accelerated warming during the past two decades. There is new and stronger evidence that most of the warming over the last 50 years is attributable to human activities. Human activities have altered the chemical composition of the atmosphere through the buildup of greenhouse gases – primarily carbon dioxide, methane, and nitrous oxide. The heat-trapping property of these gases is undisputed although uncertainties exist about exactly how earth's climate responds to them. (source:US-EPA)

Is the climate becoming warmer and warmer?

Global temperature trendNote that these are surface temperatures and mostly overland. The temperature in upper levels may be different, even reversed.

What’s the difference between “global warming” and

“climate change”?

GLOBAL WARMING is the increase of

the Earth’s average surface temperature due to a build-up of greenhouse gases in the atmosphere.

CLIMATE CHANGE is a broader term

that refers to long-term changes in climate, including average temperature and precipitation.

Difference

How Global Warming Works

Fossil fuels (coal, oil, natural gas)

Carbon Dioxide (CO2)

Why is global warming happening?

Burning of Fossil Fuels

Pollution from coal, natural gas, and oilPollution from coal, natural gas, and oilPollution from coal, natural gas, and oil

There is a direct correlation between the measured human emissions of greenhouse gases, the rise in atmospheric greenhouse gases, and the rise in temperature. The rates of increase in each is unprecedented.

There is a direct correlation between the growth in the human population and the rise in greenhouse gases and temperature.

Computer simulations indicate that only human-caused emissions of greenhouse gases can cause the observed rise in temperature of the atmosphere and other Earth systems (Oceans, Continents and Ice).

No other natural causes can account for the present rapid rise in temperature and CO2. The present rate CO2 increase is about 20,000 faster than natural rates.

We Know That Humans are the Cause

Greenhouse Effect Concentration of CO2 Feedback Effect Aerosols and Soot Solar Variation

What cause the temperature of the atmosphere to go up?

Greenhouse effect

Source: Intergovernmental Panel on Climate Change240 Watt per m3

343 Watt per m3

103 Watt per m3

The Sun’s energy passes through the car’s windshield.

This energy (heat) is trapped inside the car and cannot pass back through the windshield, causing the inside of the car to warm up.

Example of the Greenhouse Effect

Carbon dioxide (CO2) Methane (CH4) Nitrous oxide (N2O) Hydrofluorocarbons (HFCs) Perfluorocarbons (PFCs) Sulphur hexafluoride (SF6)

Greenhouse gases

Source: Kyoto Protocol- Annexure A

Natural

Manmade

Temperature, CO2 Concentrations and Carbon Emissions

Global Atmospheric Concentration of CO2

Physically, via the greenhouse effect. The connection is usually made via the

use of a climate model. Control run versus scenarios. If the scenario run results show warmer

surface condition than the control, then it is plausible to suspect that the increasing CO2 concentration in the atmosphere may cause warming.

How is the CO2 increase connected to the global warming?

Feedback Effect The climate system is very complicated. A

change in one component of the system may cause changes in other components. Sometimes the changes in other components enhance the initial change, then we say that these changes have positive feedback to the system. If the changes result in the reduction of the original change, then they have negative feedback.

Both positive and negative feedback processes may exist in the climate system. In studying the global climatic change, we cannot make conclusions based on intuition, but have to take all such possible complicated effects into account. A good climate model would have treated all of them realistically.

The main positive feedback in global warming is the tendency of warming to increase the amount of water vapor in the atmosphere, a significant greenhouse gas. The main negative feedback is radiative cooling, which increases as the fourth power of temperature

Example

Aerosols exert a cooling effect by increasing the reflection of incoming sunlight. The effects of the products of fossil fuel combustion have largely offset one another in recent decades, so that net warming has been due to the increase in greenhouse gases such as methane.

Aerosols and Soot

Atmospheric soot aerosols directly absorb solar radiation, which heats the atmosphere and cools the surface.

Atmospheric soot always contributes additional warming to the climate system.

How is global warming measured?

Ice Core Data

CO2 Measurements Before 1958 - Antarctica

Rising Sea Level Increased Temperature Habitat Damage and Species Affected Expansion of subtropical deserts Change in the amount and pattern of precipitation Extreme weather events Species extinctions

Effects of Global Warming

Effects of Global WarmingIncreased Temperature

Habitat Damage and Species Affected

Changes in Water Supply

Rising Sea Level

Alaska

Portage Glacier

1914 2004

Photos: NOAA Photo Collection and Gary Braasch – WorldViewOfGlobalWarming.org

Arizona

Colorado River

June 2002 Dec 2003

Ice shelves of the South Pole have partly separated and are collapsing. (NASA)

Receding high mountain glaciers

Melting ice and rising sea level

Of course the physical environmental change will lead to changes in the biosphere – including our society.

2007Goal: Reductions in CO2 Per Year

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Produce electricity efficientlyUse electricity efficientlyVehicle efficiencySolar and Wind PowerBiofuelsCarbon capture and storage

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What’s being done now to reduce our emissions?

Solar Power Wind Power Fuel-Efficiency

Turn off your computer or the TV when you’re not using it.

Take shorter showers. Heating water uses energy. Keep rooms cool by closing the blinds, shades, or curtains.

Turn off the lights when you leave a room.

Use compact fluorescent bulbs.

Simple Things To Do

Dress lightly when it’s hot instead of turning up

the air conditioning. Or use a fan. Dress warmly when it’s cold instead of turning up the heat. Offer to help your parents keep the air filters on your AC and furnace clean. Walk short distances instead of asking for a ride in the car.

Plant a tree.

Simple Things To Do

Recycle.

Be Bulb Smart—Use CFLs

IncandescentCompact

Fluorescent

500 lbs. of coal

What’s the difference?

•1,430 lbs. CO2 pollution avoided •$30 saved

Intergovernmental Panel on Climate Change www.wikipedia.com

References