The Earth and its atmosphere. The large H 2 O greenhouse effect is controlled by temperature – H 2 O saturation doubles with every 10°C Increase As a.

Slides:



Advertisements
Similar presentations
Climate Change and the Oceans
Advertisements

Solar Radiation and Insolation
1.Greenhouse Effect 2.The CO 2 Cycle, Long-Term Climate Change 3.Ice Ages and Short-Term Climate Change 4.Human-Induced Climate Change.
The Truth about Global Warming As seen through the eyes of a physicist Dr. Suzanne Willis, Ph.D Northern Illinois University June 29,2011.
April 28, 2009 Global Warming PPT Volvo Factory W/S Short Video.
Global Warming ‘Political hype or reality?’ The Fernhurst Society - 5 April John Clement.
Future climate (Ch. 19) 1. Enhanced Greenhouse Effect 2. CO 2 sensitivity 3. Projected CO 2 emissions 4. Projected CO 2 atmosphere concentrations 5. What.
Many past ice ages were caused by… 1.Volcanic activity 2.Photosynthesis 3.Prehistoric humans 4.Changes in the earth’s orbit 5.Sun spots.
4.4 Climate Change.
Greenhouse Effect How we stay warm. The Sun’s energy reaches Earth through Radiation (heat traveling through Space)
The current causes of climate change: the human causes.
Rising Temperatures. Various Temperature Reconstructions from
10:23 AM Sanders 7.9 Greenhouse Effect Unit 7: Water Cycle and Climate.
Air Quality and Climate Change. Coal and Oil Formation Both are Fossil Fuels: remains of plants and animals that died anywhere from 400 million to 1 million.
Climate Change – 1: Background
R21 Global Warming & Greenhouse Effect Prior Knowledge: What do you know about Greenhouse Effect and Global Warming?
Earth’s Climate: Past, Present and Future Fall Term - OLLI West: week 1, 9/16/2014 Paul Belanger, Geologist/Paleoclimatologist Introductions Key principles.
Climate Change. Climate Change Background   The earth has been in a warming trend for the past few centuries   Mainly due to the increase in greenhouse.
CLIMATE CHANGE THE GREAT DEBATE Session 10. CLIMATE CHANGE? If we have learnt anything from this course, it is that climate is not constant It is, and.
CHAPTER 16: GLOBAL WARMING. Global Change Changes in environmental processes affecting the whole Earth Temperature changes in the last decade. Which part.
Climate Climate = characteristic weather of a region. Ex. 100 year pattern. Major Elements: Temperature Precipitation (Moisture)
Weather Condition of the atmosphere at any particular time and place Air temperature, air pressure, humidity, clouds, precipitation, visibility, wind Climate.
4/23/15 The "Carbon Bathtub" Bob Powell, Ph.D. physics, MBA exponentialimprovement.com.
Samayaluca Dune Field, south of Juarez, Chihuahua Global Climate Change.
 Climate change is a significant and lasting change in the weather patterns over periods ranging from decades to millions of years.
Heating of the Atmosphere
Global warming and climate change – the causes. Temperatures are rising.
From 2010 Colorado Utilities Report FuelCO2 (lbs) per mBTU Coal215 Diesel and heating oil161 Gasoline156 Propane139 Natural gas117 Source: US EIA.
Climate change – “science catfight” or not?. The Record Of Climate Change Proxy Data.
Greenhouse Gases & the Greenhouse Effect. General Information Greenhouse gases (GHG) were naturally found in the environment before the industrial revolution.
Climate Change Pre-Quiz 1.What is the “greenhouse effect”? 2.What are examples of greenhouse gases? 3.Is climate change natural or human- made? How do.
Climate Literacy Session: Causes Peter Coombe August 5, 2015.
Global Warming (Climate Change) The Greenhouse Effect Sunlight streams through the atmosphere and heats the Earth. Some of the heat radiates back out into.
Earth’s Energy Balance Complexity, climate change and human systems HCOL 185.
Climate Change The Debate Is Done. Climate Change In the scientific world there are very few doubts about the far reaching effects of climate change The.
Projection of Global Climate Change. Review of last lecture Rapid increase of greenhouse gases (CO 2, CH 4, N 2 O) since 1750: far exceed pre-industrial.
Ch. 4-1 Role of Climate. Climate Weather – Day-to-day condition of Earth’s atmosphere at a particular time and place – What is today’s weather? Climate.
Conversations with the Earth Tom Burbine
Global Climate Change The Evidence and Human Influence Principle Evidence CO 2 and Temperature.
Climate Change: Causes and Evidence Part 1.. Climate Change What is the cause? How do we know? What is the Keeling Curve? How much CO 2 is in the atmosphere.
SC.912.E.7.2: Analyze the causes of the various kinds of surface and deep water motion within the oceans and their impacts on the transfer of energy between.
Climate Change November 4, Global Climate Change Global Warming – describes a rapid increase in the temperature of Earth’s surface, water, and atmosphere,
The Carbon Cycle and Climate Change
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
What is Climate Change?. Climate change refers to any significant change in the measures of climate lasting for an extended period of time. In other words,
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
4.4: Climate change. Changes in Carbon Dioxide in our Atmosphere in the last 100+ years. Why has carbon dioxide increased? Carbon Dioxide Levels (ppm)
CLIMATE CHANGE. CLIMATE IS: Long term Wide area Seasonal changes Measured over long spans of time CLIMATE is the average of many years of weather observation.
Climate and Human Activity. Recall Natural Greenhouse Gases.
Syed Mujeeb Ur Rahman. Student of preparatory year program the Aga Khan University Date:4/16/2010.
Global Warming Vs Climate Change
Write down 5 key words to summarise these pictures.
How Convection Currents Affect Weather and Climate.
Section Climate Change According to NASA’s Goddard Institute for Space Studies, 2009 tied for second warmest year on record, just behind The.
Climate Change Today 1.Is it Really Changing? 2.If so, are Humans the Cause?
Climate Change. Causes Several factors affect global climate: 1.Changes in solar output 2.Changes in Earth's orbit 3.Changes in the distribution of continents.
Chapter 19 Global Change.  Global change- any chemical, biological or physical property change of the planet. Examples include cold temperatures causing.
The Greenhouse Effect on Climate Change.  1. The sun’s rays warm up the land and the water.  2. Infrared rays bounce back to space.  3. Some are trapped.
Aim: How do increased carbon dioxide concentrations on our planet affect life?
Cloud formation and Atmospheric CO2. Cloud Formation There are a few ways clouds form 1.Rising Hot Air 2.Warm air over a cold body of water 3.On Mountainsides.
Greenhouse Effect How we stay warm. The Sun’s energy reaches Earth through Radiation (heat traveling through Space)
Climate Change and Earth
Greenhouse Effect Presented By: Janet Fang Sam Atwood EESC W4400.
Chapter 15.
Weather vs. Climate What’s the Difference?.
Unit 8 Notes: Climate Change
Signs of Climate change
Topic Climate Change.
Interactions between the Oceans and the Atmosphere
Presentation transcript:

The Earth and its atmosphere

The large H 2 O greenhouse effect is controlled by temperature – H 2 O saturation doubles with every 10°C Increase As a result It is concentrated in the lower atmosphere of the tropics The most potent greenhouse gas is H 2 O - vapor

The CO 2 greenhouse gas effect is concentrated in the polar regions ! ! ! CO 2 is evenly distributed throughout the atmosphere Particularly in the Arctic !

John Cook, from IGPP 2007 data; ~93% to oceans continues (NOAA/NODC, 2012) Melting ice absorbs ~2% Only ~2% stays in atmosphere ~2% warms the land

Oceans, m depth Oceans, m depth Atmosphere + land + ice melting Change in heat content, (NOAA 2012 data, Nuccitelli et al plot) 5-year moving averages Joules ( Increasing heat, not shown, goes deeper than 2000 m)

m 3 (95 cm x 95 cm x 95 cm)

10 o C = (50 o F) 7.8 cc 20 o C = (68 o F) 15 cc 30 o C = (86 o F) 27.7 cc 40 o C = (104 o F) o C +1 o C = 8% increase in vapor

Climate Changes from Ocean Sediment Cores, since 5 Ma. Milankovitch Cycles 41K 100 K 3.0Ma 4.0Ma 2.0Ma 1.0Ma5.0Ma 0 When CO 2 levels get below ~ ppm Orbital parameters become more important than CO 2 the last time inferred temperatures will have been this high – once equilibrium is reached, will have been 3-5 million years ago or more * we are now about here

China has the largest fossil fuel emissions today. However, climate change is driven by cumulative emissions, so developed nations, especially the U.S., have greatest responsibility.