Insolation and Earth: A Dynamic Relationship

Slides:

Advertisements

Similar presentations

Heat Transfer. 1. The emission of energy in waves. 2. Heat transfer through contact. 3. Heat transfer through circulation due to differences in density.

Advertisements

Heating of the Atmosphere

Solar Radiation and Insolation

An improved energy balance model: Atmosphere and Greenhouse gases

1. Try to produce a flow chart from the text I read to you 2. Look at pages 208 to 209 of David Waugh and answer the following; a) Describe how the.

Climate Earth’s Radiation Balance. Solar Radiation Budget Life on earth is supported by energy from the sun Energy from the sun is not simply absorbed.

Solar constant The solar constant is the amount of incoming solar radiation per unit area, measured on the outer surface of Earth's atmosphere, in a plane.

3. Climate Change 3.1 Observations 3.2 Theory of Climate Change 3.3 Climate Change Prediction 3.4 The IPCC Process.

Lecture 3: The greenhouse effect. Other concepts from Lecture 2 Temperature Scales Forms of Heat Transfer Electromagnetic Spectrum Stefan-Boltzmann Law.

Outline Further Reading: Chapter 04 of the text book - matter-energy interactions - shortwave radiation balance - longwave radiation balance Natural Environments:

1 Weather and Climate Bay Area Earth Science Institute (BAESI) Energy in the Atmosphere San Jose State University, January 24, 2004

the Natural Greenhouse Effect

1 BAESI - Global Warming: Food Climate Connections The Greenhouse Effect Dr. Eugene Cordero San Jose State University Outline  Greenhouse effect  Energy.

Incoming Solar Energy What affects the amount of incoming solar energy?

The Greenhouse Effect 3/3/ b pgs IN: What do you think is the Greenhouse Effect? Put your Lesson 12 on the books.

Global Warming and the Greenhouse Effect Climate and Climate Change.

What exactly is a budget? Do you or your parents have a budget? Definition: budg·et an estimate of income and expenditure for a set period of time.

Atmosphere Structure & Compostion

Absorption of Insolation by the Atmosphere

Earth Science The Greenhouse Effect November 10, 2011 R. Alvarez.

Understanding the Greenhouse Effect Sara Kalinowski and Ellen Cercena.

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.

Greenhouse Gases and Energy Budget LP 3 1. What are greenhouse gases? Where do they come from? How do they work? 2.

Solar Radiation and Insolation Incoming solar radiation:

The Atmosphere: Energy Transfer & Properties Weather Unit Science 10.

Insolation and the Greenhouse Effect Energy in Earth’s Atmosphere.

Topic 6. Without energy from the sun, conditions on Earth would be different. What is the energy that is radiated from the Sun? The energy that is radiated.

The Radiation Budget and the Greenhouse Effect SNC2D.

UNIT 8 Biology and Geology 4. Secondary education Ecosystems III: ecological balance THE GREENHOUSE EFFECT.

Atmosphere Earth’s albedo. AtmosphereEarth’s albedo “Describe and explain the energy exchanges that result in the Earth’s surface receiving only 56% of.

WHERE DOES THE INCOMING SHORTWAVE RADIATION GO TO? The Shortwave Radiation Balance.

INSOLATION Incoming Solar Radiation Portion of sun’s output of electromagnetic radiation that is received by earth.

Greenhouse Effect Sun Earth’s Temperature Solar Energy Solar Energy Solar Energy Solar Energy.

The Greenhouse Effect. Natural heating of earth’s surface caused by greenhouse gases –CO 2 (Carbon Dioxide) –CH 3 (Methane) –N 2 O (Nitrous Oxide) –H.

Atmospheric gases allow sunshine to pass through but absorb heat that is radiated back from the surface of the earth. This acts as a blanket keeping heat.

Aim: How is INSOLATION described? Do Now: What is the least and the most hours of daylight during the year?

TOPIC 6 INSOLATION.

Global energy balance SPACE

Natural Environments: The Atmosphere

Incoming Solar Radiation

What is INSOLATION? A Science Sisters Production 2017.

Energy from the Sun Sun’s energy travels 148 million km to Earth in only 8 minutes Earth receives less than one-billionth of the Sun’s energy Reaches Earth.

What controls climate? Energy from the Sun – Radiation

Miss. Jadhav S.V. Assit.Professor

Unit 3 Notes Part 4: Greenhouse Effect

Energy Budget Subtitle.

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.

QUIZ 3 #1. What does this represent? Incoming shortwave

Energy Balance and Circulation Systems

Geography Atmosphere Introduction to the Atmosphere [Date] Today I will: - Be introduced to the layers of the atmosphere and the global heat budget.

Atmosphere Thinking Sheet 1/30/18 or 1/31/18

Energy in the Atmosphere

ATOC 4720 class27 Radiative transfer in global energy balance

What controls climate? Energy from the Sun – Radiation

Earth’s Energy Budget.

Global Change: Class Exercise

Global Change: Class Exercise

Energy transfer in the atmosphere

Journal #25 What is a greenhouse? What is the greenhouse effect?

Energy from the Sun.

LO: What is Insolation? Do Now: In your notes write what you think Insolation is. Grab Plicker cards.

Climate Change.

Can you think of any temperature patterns on Earth?

Topic 6 Insolation and the Seasons

Energy in the Atmosphere

SOLAR BUDGET AND ALBEDO

The Ins & Outs of Solar Radiation

Global Change: Class Exercise

Unit 5 Earth’s Energy Budget.

Energy in the Earth’s Atmosphere

Presentation transcript:

Insolation and Earth: A Dynamic Relationship Earth Science Mr. Cloud

What makes a planet habitable? What criteria do astronomers use to gauge if an newly discovered exoplanet is habitable?

Why is insolation so important?

INSOLATION! Insolation Break down the word! In – incoming sol – solar ation- radiation INSOLATION!

Interaction of Insolation with the Environment Insolation interacts with the environment in three main ways: Absorption Reflection Scattering

The Interaction of Earth’s Atmosphere with Insolation

The Greenhouse Effect Insolation penetrates Earth’s atmosphere and gets absorbed by Earth’s surface The Earth re-radiates energy in the form of infrared, long wavelength radiation. Greenhouse gases (H2O(v), CO2, CH4) absorb some of the outgoing radiation.

Radiative Balance Withdraw $1.50 Withdraw $1.50 Deposit $1.50