Radiation Balance and Feedbacks

Slides:



Advertisements
Similar presentations
What? Remote, actively researched, monitored, measured, has a huge impact on global climate and is relatively cool?
Advertisements

CLIMATE CHANGE IMPACTS ON THE PRAIRIE Mandy Guinn, Kerry Hartman, Jen Janecek-Hartman.
Seasons.
Cheryl Gann NCSSM Instructor of Mathematics Special Thanks to Linda Schmalbeck, NCSSM Instructor of Biology, for the activity inspiration.
Climatic changes in the last 200 years (Ch. 17 & 18) 1. Is it warming? --climate proxy info (recap) -- info from historical & instrumental records 2. What.
Essential Principles Challenge
Global & Regional Climate Change Science a presentation from the CIMSS Climate Literacy Ambassadors community A low-carbon climate education project.
Albedo. 3/30 WHOT Teaching Point:  Objective: Collect data on the albedo of various surfaces on Earth.  Responsibilities: Albedo Lab Due Wednesday.
SNC2D Brennan Climate Change. Paleoclimate record Ice samples Sediment cores Pollen records Peat Bogs Fossil records Proxies –Use data that represents.
The Greenhouse Effect. What controls climate? Energy from the Sun – Radiation! Consider the 4 inner planets of the solar system: SUN 342 W m W.
Questions for Today:  What is Weather and Climate?  What are four major factors that determine Global Air Circulation?  How do Ocean Currents affect.
International Environment Forum Conference Ottawa October 12 th, 2007 John M R Stone Carleton University.
Bellwork What is the greenhouse effect? What is global warming?
Global Climate Change The Evidence and Human Influence Principle Evidence CO 2 and Temperature.
The Water Planet Chapter 2 Section 1. Water Water covers 70% of the earth’s surface Examples: Streams, Rivers, Lakes, Seas, Oceans, Water Vapor, Glaciers,
Climate Change Monday, November 5th. Anthropogenic Climate Change Thomas Jefferson, 1781 Notes on the State of Virginia –Springs are warmer –Less winter.
Class #39: Friday, April 171 Mechanisms of Climate Change Natural and Anthropogenic.
Grade 8 Science Warden Ave PS. Learning Goals By the end of this presentation we will be able to: Describe various effects water has on weather patterns.
Ice Loss Signs of Change. The Cryosphere  Earth has many frozen features including – sea, lake, and river ice; – snow cover; – glaciers, – ice caps;
Chapter 23 The Atmosphere, Climate, and Global Warming.
To recap Give 2 examples of research methods that show long term historical climate change? How reliable are these? Give 2 ways of measuring medium term.
Increase Your Albedo! Exploring the Fate of Arctic Sea Ice.
Atmospheric Heating.
The Water Cycle.
Chapter Thirteen: Atmosphere and Climate Change
TOPIC 6 INSOLATION.
Climate Change Climate – The average year after year pattern of temperature, precipitation, winds and clouds in an area. Climates are classified mainly.
Get ready to move seats. Again...
Evidence of a Changing Climate
Climate Change slides for Exam Two
The Greenhouse Effect 8.6 The greenhouse effect is a natural process whereby gases and clouds absorb infrared radiation emitted by Earth’s surface and.
14.8 NOTES Greenhouse Gases
Principles of the Global Climate System II
8.10 Feedback Loops and Climate
Earth and Human Activity
Natural Causes of Climate Change
Powering Earth’s Climate
WEATHER.
Atmosphere and Weather
14.3 – NOTES Thermal Properties
Weather Chapter 16 Notes.
IPCC Climate Change 2013: The Physical Science Basis
Climate: Earth’s Dynamic Equilibrium, Part 2
ENERGY IN THE BIOSPHERE
Global Climate Change.
Climate Change.
Intergovernmental Panel on Climate Change
L.O: SWBAT explain THE GREEN HOUSE EFFECT Do Now:11 &13.
Water on Earth.
Fig. 2 shows the relationship between air temperature and relative humidity. (a) (i) Describe the relationship shown in Fig. 2. [3] (ii) State.
THE WATER CYCLE The Water Cycle.
Composition, Structure, & Heat Budget
Water on Earth.
Standard 4-1 Workbook “The Water Cycle” Page 6
THE WATER CYCLE the continuous movement of water on, above, and below the surface of the Earth.
Climate and Change.
FIGURE 2.10 Sunlight warms the earth’s surface only during the day, whereas the surface constantly emits infrared radiation upward during the day and at.
The Water Cycle.
The Water Cycle.
Seasons.
Climate and Seasons Notes
“ What Causes Our Weather”
Signs and impact of Global Climate Change
Water on Earth.
Climate Earth’s Energy Budget.
The Hydrosphere and the Biosphere
What causes our Weather?
States of water (review) (section 10.1)
Atmosphere and Climate Change
“ What Causes Our Weather”
Presentation transcript:

Radiation Balance and Feedbacks

Differences New - Old Absorbed by atmosphere 79/67 = 18% increase Reflected by Surface 24/30 = 20% decrease Total reflection = 107/100 = 7% decrease “Back Radiation” = 342/324 = 5% increase go more “global warming”

One way to think about Climate Change is an intensification of the water cycle As the temperature of the atmosphere rises, more water is evaporated from ground storage (rivers, oceans, reservoirs, soil). Because the air is warmer, the relative humidity can be higher, and the atmosphere can 'hold' more water vapor. As a greenhouse gas, the higher concentration of water vapor is then able to absorb more thermal IR energy radiated from the Earth, thus further warming the atmosphere. The warmer atmosphere can then hold more water vapor and so on and so on. This is referred to as a 'positive feedback loop'. In a warming climate, water vapor plays a major role in a positive feedback loop that amplifies global climate change. (H20 responds to changes in climate, but it doesn’t drive climate change)

No Evidence of “recent” increasing cloud cover

Observed warming is consistent with observed changes: There is a widespread retreat of nonpolar glaciers. Arctic sea-ice has thinned by 40% in recent decades (summer & autumn) And decreased in extent by 15% since the 1950s in spring and summer. Northern Hemisphere snow cover has decreased by 10% since the 1960s. The growing season has lengthened by about 1 to 4 days per decade during the last 40 years in the Northern Hemisphere, especially at higher latitudes. The duration of ice cover on lakes decreased by about 2 weeks over the 20th century in mid- and high latitudes of the Northern Hemisphere. The global mean sea level has increased at an average annual rate of 1 to 2 mm during the 20th century.

Closer Look at Climate System

Climate Feedback Mechanisms