Cooperation of international societies to carry out the Forced Thickening of Ice against Global Warming Cooperation of international societies to carry.

Slides:



Advertisements
Similar presentations
CLIMATE SYSTEMS.
Advertisements

Michael B. McElroy ACS August 23rd, 2010.
The syllabus says: Atmosphere and change  Describe the functioning of the atmospheric system in terms of the energy balance between solar and long- wave.
Earth’s radiative balance or, how I learned to stop worrying and love the greenhouse effect If the Earth had no atmosphere: T  T 4 = S / 4 (1 — A) T =
Global Warming and Climate Sensitivity Professor Dennis L. Hartmann Department of Atmospheric Sciences University of Washington Seattle, Washington.
What are aerosols ? Aerosol is a collection of particles suspended in the air, they range in size from 0.01 microns to several tens of microns.
What is Climate? Section 16.1 Pg Climate Is the characteristic weather of a region Includes: temperature, precipitation, air pressure, humidity,
Ocean and Climate An Introduction Program in Climate Change Summer Institute Friday Harbor Labs September 2008 Dennis L. Hartmann Atmospheric Sciences.
Global Warming Causes and Mechanics. What is Global Warming? “The recent increase in the world's temperature that is believed to be caused by the increase.
Solar Energy Solar energy is the source of most of Earth’s heat on land, in the oceans and in the atmosphere. When solar energy interacts with air, soil.
CHAPTER 5. * Weather is daily changes in temp and precipitation. * CLIMATE is the average year to year conditions.
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 UNIT 3 Chapter 7: Earth’s Climate System
Atmosphere and Climate Change
The Atmosphere & Climate
Climate. Weather vs. Climate Weather- State of the atmosphere at a given time and place; constantly changing Climate – The average weather condition of.
Earth Science Chapter 11.2 Climate Change.
Physical Science 22 Characteristics of the Atmosphere.
Global Warming Inez Fung University of California, Berkeley April 2007.
HEAT TRANSFER & The NATURAL GREENHOUSE EFFECT. TRAPPING HEAT  A “ greenhouse ” is any structure that is designed to take in the sun’s energy and trap.
Ch : Climate & Climate Change Objectives: 1
Chapter 18 – Climate and Climate Change
Climate Change: From Global Predictions to Local Action Mathematical Sciences Research Institute April
Heating of the Atmosphere
WEATHER or CLIMATE? Can you tell the difference? Put these words in to two lists under the headings ‘Weather words’ and ‘Climate words’ Cold winters Cloud.
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.
5-5. GLOBAL WARMING Introduction  Definition:  Rise in the average temperature of the Earth’s surface (mainly air T).  From the Environmental.
Attendance Climate Questions Climate Review Sheet answers You have a test tomorrow that is worth 40% of your grade.
S6E2.c. relate the tilt of earth to the distribution of sunlight through the year and its effect on climate.
AOS 100: Weather and Climate Instructor: Nick Bassill Class TA: Courtney Obergfell.
Lecture Outlines Physical Geology, 14/e Copyright © The McGraw-Hill Companies, Inc. Permission required for reproduction or display. Plummer, Carlson &
The Atmosphere Atmosphere- A thin layer of gases that surrounds the Earth –78% nitrogen –21% oxygen –1% water vapor, argon, carbon dioxide, neon, helium.
Albedo varies with season and geography Surface cover that has a high albedo Snow & ice Cloud cover Aerosols 
Heat Energy Transfer SNC2D.
2. The Hydrosphere liquid water, water vapour & clouds absorb energy from warm air and the Sun, and then release it back. also reflects some of the Sun’s.
What is Climate?.
Human fingerprints on our changing climate Neil Leary Changing Planet Study Group June 28 – July 1, 2011 Cooling the Liberal Arts Curriculum A NASA-GCCE.
Arctic and Antarctic Review Glacier Arctic Global WarmAntarctic Misc Q $100 Q $200 Q $300 Q $400 Q $500 Q $100 Q $200 Q $300 Q $400 Q $500 Final Jeopardy.
Insolation and the Greenhouse Effect Energy in Earth’s Atmosphere.
Composition of the Atmosphere  A mixture of chemical elements and compounds: –Nitrogen (N 2 ) ~ 78% –Oxygen (O 2 ) ~ 21% –Other gases ~ 1%
WATER: Let’s Get Thirsty for Life! Water Distribution
UNIT 3 Climate Change 1.
 What is your view on climate change? Write down either: What you believe about climate change What you have heard someone say about climate change 
TOPIC 6: GLOBAL WARMING AND GREENHOUSE EFFECT. Temperature and Carbon Dioxide Concentration from 1880 to present.
Section - 01 cont’d Lesson 2 Temperature and Heat.
Earth’s climate and how it changes
Heat in the Atmosphere The sun’s energy is transferred to earth and the atmosphere three ways Radiation, Convection and Conduction.
Chapter 13 Section 3 Global Warming Environmental Science Spring 2011.
L- Latitude O- Ocean Currents W- Wind and Air Masses E- Elevation R- Relief N- Nearness to Water.
How Convection Currents Affect Weather and Climate.
Climate Change. Natural Processes That Change Climates  Volcanic Eruptions  The presence of volcanic aerosols (ash, dust, and sulfur-based aerosols),CO.
8.4 Components of Earth’s Climate System. 4 main components 1 - Atmosphere: layers of gases 2 - Hydrosphere: all water, salt, fresh & frozen 3 - Lithosphere:
C LIMATE Chapter 21. F ACTORS THAT A FFECT C LIMATE Latitude Less solar energy as you move away from the equator Tropical zones Rays from the sun hit.
Climate. Weather vs. Climate Weather – the condition of Earth’s atmosphere at a particular time and place. – Short-term: Hours and days – Localized: Town,
Cloud Formation. Review LCL & Dew Point The Sun’s radiation heats Earth’s surface, the surrounding air is heated due to conduction and rises because of.
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.
Meteorology Chapter 17. Chapter 17.1 While you read 1.Volcanic eruptions  lowered temperature 2.Volcanic eruptions  released gases to form atmosphere.
Chapter 4: Weather and Climate Notes
What is Climate?.
Changes in the Atmosphere
5.1 What is Climate? 5.2 Climate Zones
Climate Vocabulary Terms you need to know!.
What is Climate?.
Atmosphere and ocean interactions
Human Impacts on Climate Change
Place these answers onto your Meteorology Chapter 17 Worksheets.
Global = whole earth Warming= temperature going up
Greenhouse.
Climate.
Presentation transcript:

Cooperation of international societies to carry out the Forced Thickening of Ice against Global Warming Cooperation of international societies to carry out the Forced Thickening of Ice against Global Warming Prof. Hi-Ryong BYUN President, Korean Meteorological Society Dept. of Env. Atmospheric Sciences, Pukyong National University 3 Nov. 2011

1. Reflection of solar energy at stratosphere or in troposphere by mirrors or aerosols. 2. Sequestration of CO2 from fossil fuel combustion. 3. Ocean surface fertilization. 4. Afforestation. => 1. Most of them have harmful side effects. 2. They need long time (100 years?) to reduce global temperature after normalization of CO2. One simple technique that has no harmful side effects, that can reduce global temperature as soon as it operates, and that it needs international cooperation. => It is the forced thickening of ice Techniques of Geo-Engineering Techniques of Geo-Engineering

There are long duration without ice over the sea, though both of air and water temperature are below zero. => Let’s use this nature to stop global warming.

1. Reflection of solar energy at stratosphere or in troposphere by mirrors or aerosols. 2. Sequestration of CO2 from fossil fuel combustion. 3. Ocean surface fertilization. 4. Afforestation. => 1. Most of them have harmful side effects. 2. They need long time (100 years?) to reduce global temperature after normalization of CO2. One simple technique that has no harmful side effects, that can reduce global temperature as soon as it operates, and that it needs international cooperation. => It is the forced thickening of ice Techniques of Geo-Engineering Techniques of Geo-Engineering

Positive feedback mechanism of sea ice formation Positive feedback mechanism of sea ice formation 1. The wider the ice cover over sea is, the more sunshine reflects. Albedo of Ice = 0.6~0.9 Albedo of water = 0.08 Albedo of water = 0.08 => Air becomes cooler. => Air becomes cooler. 2, The cooler the air becomes, the more the ice forms. 2, The cooler the air becomes, the more the ice forms. 3. This is positive feedback => It will stop global warming. 3. This is positive feedback => It will stop global warming.

Procedure of Forced Thickening of ice Procedure of Forced Thickening of ice Method Spray cold water over sea surface and get an ice plate on sea surface. 2. Ice will glow upward by rain and snow and downward attaching the fresh water in sea during the whole winter.

Procedure of Forced Thickening of ice Procedure of Forced Thickening of ice Method Raise sea water from sea surface and exposure it to cold air. => water freeze to ice plate => drop the ice plate to water and raise another water. = Continuous operation. 0. Ice will glow upward by rain and snow and downward attaching the fresh water in sea during the whole winter. => Same effects with method 1.

Effects Effects 0. FTI is possible from Nov. till May (5 months) => More ice can be made. 0. Original ice bergs do not melt during summer because of this man-made ice. 0. The Earth absorb an additional energy of 0.85 Wm -2 by global warming (Hansen et al., 2005)=> This warming will stop when additional 4.8 * 10 6 km 2 were covered with ice. This is 40% of total area above 35 Latitude (N and S) (Byun et al., 2008). 0. International cooperation is needed to widen ice cover over sea for stopping of global warming. 0. IFMS is the best society to capture global warming.

The End The End Thank you!! Thank you!!