The Earth’s Atmosphere. GasPercent Nitrogen78% Oxygen21% Argon0.93% Carbon Dioxide (CO 2 ) 0.037% Neon, helium methane, ozone… ~0.04% Also water vapor.

Slides:



Advertisements
Similar presentations
THE ATMOSPHERE.
Advertisements

Energy Transfer Atmosphere Global Warming Did you read? Say What? 100
Heat Transfer, Greenhouse Effect, Ozone Layer Notes
Earths Atmosphere.
 Extends from the Earth’s surface to outer space.  About 900 km (560 miles)  Mixture of gases, solids, and liquids.
Objectives Describe the composition of Earth’s atmosphere.
Weather JEOPARDY Heat Energy Air Pressure Greenhouse Effect The Atmosphere
Chapter 2: Weather Factors
ENERGY FROM THE SUN Chapter 14.3 Pages Energy in the Atmosphere The sun is the source of ALL energy in our atmosphere. Three things that can.
Earth’s Changing Atmosphere. Main Topics Definition and Characteristics of the Atmosphere Changes to the Atmosphere composition Layers of the Atmosphere.
Chapter 3 Section 2.
Earth’s Atmosphere Why is it so important to life on Earth?
Chapter One: The Atmosphere
Basic Properties of the Atmosphere
The Atmosphere “Vapor Globe/Ball”. Composition  78% Nitrogen  21% Oxygen  1% Other (Argon, Carbon Dioxide, Water Vapor, other gases)  78% Nitrogen.
Heating of the Atmosphere
Atmosphere Chapter 11 Notes. Composition of the Atmosphere Currently: – Nitrogen (N 2 ): 78% – Oxygen (O 2 ): 21% – Argon (Ar) – Carbon dioxide (CO 2.
The Greenhouse Effect Too much of a good thing?. Light from the sun is composed of many frequencies.
The Greenhouse Effect (8.6). The Greenhouse Effect  How does the climate system trap energy to keep Earth warm?  Gases in the atmosphere absorbed the.
4.6 billion years old Will last another 5 billion years Made mostly of Hydrogen and Helium Goes through fusion to combine Hydrogen into Helium. This.
Chapter 1 The Atmosphere Section 1 The Air Around You
Ch 17 Section 1 Earth’s Atmosphere. Atmospheric Composition Air is comprised of 78% Nitrogen, 21% Oxygen and trace amounts of CO 2, Argon, and water vapor.
Energy in the Atmosphere
Weather Review. Air Masses Air Mass – A large body of air through which temperature and moisture are the same. Types 1. Continental – formed over land.
1._____gases that surround the Earth and keep it warm and wet 2._____layer that meteors burn up in 3._____bottom layer of the atmosphere RAP.
Mr. Fleming. The trapping of heat from the sun by gases in the Earth’s atmosphere. The major gas contributing to this process is Carbon dioxide gas.
The trapping of heat from the sun by gases in the Earth’s atmosphere. The major gas contributing to this process is Carbon dioxide gas. Greenhouse effect.
Solar Energy Heat and Light. Energy Can take many different forms –____________ –Heat –____________.
Heat Transfer in the Atmosphere Essential Question: How is heat transferred in the atmosphere?
The Atmosphere By : Jennifer Drinkard. Atmospheric gases Our atmosphere is made up of mainly Nitrogen, Oxygen, and Carbon Dioxide, but it also contains.
What processes heat the atmosphere?
Learning Intention Understand the driving forces of weather and climate.
Section 1.3 Gases in the atmosphere absorb radiation.
Journal #18 What is the atmosphere? What do you think it is made of? What do you think makes up air?
The Dynamic EarthSection 2 Objective #9 Describe the layers of the Earth’s atmosphere.
Earth’s Atmosphere intro intro. Atmospheric Composition Gas% Nitrogen78% Oxygen21% Argon0.9% Carbon Dioxide0.04% Other Gases, Dust and Water Vapor 0.06%
Greenhouse Effect Sun Earth’s Temperature Solar Energy Solar Energy Solar Energy Solar Energy.
Atmospheric Heating Radiation Conduction Convection.
If it were not for greenhouse gases trapping heat in the atmosphere, the Earth would be a very cold place. Greenhouse gases keep the Earth warm through.
Atmosphere. Earth’s Radiation Budget Earth maintains an energy balance and a temperature balance by radiating as much energy into space as it absorbs.
DAY 1 Chapter 3 The Dynamic Earth Section 2: The Atmosphere.
Section 3.2 The Atmosphere
ATMOSPHERE NOTES September 2, What is weather?  Weather is the condition of Earth’s atmosphere at a specific time and place.
CHAPTER 19 HEAT TRANSFER IN THE ATMOSPHERE. WHAT IS THE ATMOSPHERE? Earth’s atmosphere is heated by the transfer of energy from the sun. Some heat comes.
Atmospheric Heating.
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.
Heat in the Atmosphere.
Composition & Structure
Earth’s Climate System and Natural Change
Atmosphere.
Earth’s Changing Atmosphere
The Atmosphere.
The Earth’s Atmosphere
the Atmosphere’s Role in Weather
The Atmosphere Thin layer of gases that surrounds Earth.
Weather The condition of Earth’s atmosphere at a particular time and place.
The Atmosphere Earth’s atmosphere is a mixture of gases that distributes heat and enables life to exist on Earth.
Weather and Climate: Earth’s Atmosphere
Earth's atmosphere reflects or absorbs some sunlight but allows most of the visible light pass through to Earth's surface. 4 ways the atmosphere affects.
The Atmosphere.
Section 2 Atmospheric Heating.
The Air Around You Notes
Atmosphere The Basics.
Earth's Atmosphere Troposphere Stratosphere
Layers of the Atmosphere
Climate Change.
Air Pollution.
Earth's atmosphere reflects or absorbs some sunlight but allows most of the visible light pass through to Earth's surface. Atmosphere affects light in.
Atmosphere 1.3 RSG-B Answers.
The Atmosphere.
Presentation transcript:

The Earth’s Atmosphere

GasPercent Nitrogen78% Oxygen21% Argon0.93% Carbon Dioxide (CO 2 ) 0.037% Neon, helium methane, ozone… ~0.04% Also water vapor (most near the surface of the earth), dust and pollutants (e.g. sulfur dioxide)

0.039% means 390 ppm (“ppm” = parts per million) Pre-industrial CO 2 level: 275 ppm Present CO 2 level: 390 ppm Safe (?) CO 2 level: 350 ppm A Special Note on Carbon Dioxide present in trace amounts, but important in its effects: a greenhouse gas (GHG) – a gas that is very effective at absorbing (trapping) and emitting radiation as heat (infrared radiation)

Why is the atmosphere important? 1.Natural Greenhouse Effect, temperature extremes: warms Earth’s surface, reduces day/night extremes; 2.Ozone layer: protects against damaging ultraviolet (UV) radiation from the Sun; 3.Water Cycle: movement of water - evaporation, transpiration from plants, precipitation - provides for life;

Convection cells: Warm moist air rises at equator; Cold dry air sinks at the poles; Gives rise to winds; Heat Energy and moisture: Transfers heat and moisture around the globe, to the poles; Atmospheric Circulation

Atmospheric Layers