Global warming: Is the Sun heating the Earth? Lecture 8: The Sun-Earth Connection

Size: px
Start display at page:

Download "Global warming: Is the Sun heating the Earth? Lecture 8: The Sun-Earth Connection"

Transcription

1 Global warming: Is the Sun heating the Earth? Lecture 8: The Sun-Earth Connection

2 Solar influence on Earth The variable activity of the Sun affects Earth in many ways: short term long term Space weather : Disturbances in the Magnetosphere, Ionosphere, Upper atmosphere Satellite systems, Communication and Energy supply Global climate change Modulation of galactic cosmic rays hitting Earth

3 Space weather Cause: variability of Sun & solar wind (CMEs, flares, high speed wind streams) Solar components: solar energetic electro-magnetic (UV, X- rays, γ-rays) & particle radiation (ev to MeV) Affected natural systems: Earth s magnetosphere, ionosphere, thermosphere, stratosphere Technical systems in space & partly on Earth affected Potential health hazard: astronauts, airplane passengers & crew, inhabitants at high latitudes (ozone hole)

4 Causes of space weather Variations of solar electromagnetic radiation, specially UV- and X-radiation Solar wind Suprathermal particles (energies of ev) Energetic particles (kev to MeV) From Sun Cosmic rays (MeV to GeV) Meteorites, interplanetary dust, galactic Gamma-Ray-Bursts, etc. Other sources

5 The Sun and space weather: CMEs Composite of Sun and its extended corona (LASCO C2 + C3 EIT 304 Å) Bright, overexposed dots are planets (Mercury, Venus, Jupiter, Saturn), fainter background objects are stars R. Schwenn

6 Halo CMEs Halo CMEs: CMEs directed towards (or away from) Earth. The main cause of Space Weather Most difficult to detect! Most difficult to predict propagation speed.

7 Effect of a CME directed to Earth The largest solar particle events appear to result from shock associated coronal mass ejections (CMEs)

8 Space Weather: the Aurora

9 Influence of solar activity on technical systems L. Lanzerotti

10 Ionospheric heating by UV radiation Most important for Earth s upper atmosphere is Lyα: its strength changes by factor of 2 over a solar cycle Larger temperature means larger scale height: ionosphere expands drag on spacecraft increases

11 Increased Drag on Satellites Expanding atmosphere causes increased drag on low orbit satellites. They loose altitude & non-symmetrical satellites can start tumbling Skylab re-entered several years earlier than planned Hubble Space Telescope drops km per year (Re-boosted by the Shuttle More than 12 satellites lost due to Space Weather Effects HST

12 Astronaut safety The Earth s magnetosphere helps to protect the astronauts on, e.g. the ISS Astronauts flying to moon etc. are at risk SEPs are a major handicap for manned Mars mission

13 Bright Sun causes dark night Blackout in Canada and NE USA due to solar damage to transformers (2003, at last activity maximum)

14 Bright Sun causes dark night Satellite based telecommunications growing most rapidly Navigation now also largely satellite based: GPS, Galileo Satellite payloads increasingly sensitive Humans in Space: more and longer manned missions Importance of Space Weather warnings will increase

15 Bright Sun causes dark night Satellite based telecommunications growing most rapidly Navigation now also largely satellite based: GPS, Galileo Satellite payloads increasingly sensitive Humans in Space: more and longer manned missions Importance of Space Weather warnings will increase

16 Does the Sun influence climate? Answer depends on the considered time scale Time scales of billions of years: yes! The Sun s evolution makes it increasingly brighter Time scales of years: Indirectly. Ice ages are probably caused by changes in the Earth s orbital parameters Time scales of decades to millenia: Probably. There are increasing indications of a solar contribution to global climate change days to a year: Unclear

17 Evolution of solar luminosity Today Sackmann et al. 1997

18 Evolution of solar luminosity Runaway greenhouse effect through evaporation of oceans Today Sackmann et al The future of the Earth?

19 Climate evolution: the broader context The Earth today is cooler by 4-6 K than it was 10 million years ago

20 Ice ages and warm periods

21 Milankovitch theory Ice ages are due to variations of Earth s orbit The dominant parameter

22 Cause of ice ages Standard theory: Milankovitch theory of orbital parameter changes of Earth, combined with non-symmetric distribution of continents. Largest is effect of the change of the eccentricity of the Earth s orbit. It shows a good correlation with Earth s temperature

23 Has the Earth warmed? Is this warming significant and important?

24 Die Has Sonne the Earth als Klimatreiber? warmed? Klima: Beeinflusst die Sonne das Klima und trägt sie Is this warming significant and important? zum gegenwärtigen Klimawandel bei?

25 Has the Earth warmed? Is this warming significant and important?

26 Has the Earth warmed? Muir & Riggs Glaciers, Alaska Is this warming significant and important?

27 Is the Recent Temperature Rise Extraordinary? Various temperature reconstructions suggest that the Earth is hotter now than in the last 2000 years Mann et al.; Moberg et al.

28 Is Global Warming Manmade? CO 2 main man-made greenhouse gas Source: NASA

29 IPCC Predictions until 2100 Scenarios for emission of Greenhouse Gases Predicted temperature over next 100 years Expect o warming by 2050

30 Extreme weather events Some Consequences of Global Climate Change Rising sea level

31 Is everything understood?

32 Could the Sun be to blame? The Sun delivers 1.36 kw / m 2. We get 1 kw / m 2 (at equator, at noon, if no clouds) In min the Sun provides to Earth the yearly energy needs of Humanity Without sunlight, no life (Our atmosphere would cool to below -200 o C within weeks)

33 Maunder Minimum & Little Ice Age H. Avercamp The Maunder Minimum corresponded to the Little Ice Age: Is there a connection? The coldest decade in England since the 1690s; 1813/1814 last Christmas Fair on the Thames Dalton

34 Paths by which Sun can affect climate Variations of total irradiance: change in total energy input to Earth s atmosphere [irradiance] = W/m 2 = flux at 1AU (above Earth s atmosphere) Variations of UV irradiance: influence on atmospheric chemistry (e.g. stratospheric ozone production and depletion) Modulation of cosmic rays: has been proposed to affect cloud cover. Energy carried by particles at 1 AU W/m 2 (mainly protons and electrons) vs W/m 2 from radiation

35 Measured total irradiance 0.1% C. Fröhlich, PMOD

36 Measured total irradiance 0.1% C. Fröhlich, PMOD

37 During activity maximum, when the number of sunspots is largest, the Sun is also brightest. How can this be consistent with what we have seen on the last slide? Irradiance Sunspots

38 Faculae and Plage Area increase of faculae from activity min to max is factor of greater than of sunspots

39 Passage of a Facular Group

40 Evidence of influence of solar cycle irradiance variations on climate Solid line: Earth global surface temperature after removal of linear trend Dashed line: solar total irradiance Global temperature varies by 0.2 o between solar activity minimum and maximum Camp and Tung (2007), Tung and Camp (2008)

41 3- Component Model F(λ) F(λ) α (t) s F(λ) quiet Sun flux (Fontenla et al. 1993) sunspot flux; separate umbra/penumbra (cool Kurucz models) filling factor of sunspots (MDI continuum) facular flux (modified model-f; Fontenla et al. 1993; Unruh et al. 2000) α (t) filling factor of faculae f (MDI magnetograms)

42 B as source of irradiance changes Wenzler, Solanki, Krivova 2005

43 Are there longer term variations of solar irradiance? Irradiance during current minimum is lower than in earlier times No direct records of irradiance variations on longer time scales. Need to use models. Need to distinguish different periods Since ~ 1800: good direct sunspot number measurements Since 1611: telescopic sunspot number measurements On longer time scales: first a proxy of the solar magnetic field must be reconstructed.

44 Reconstruction of open flux back to Be Open solar flux Interplanetary field Solanki et al Nature Model also predicts very similar trend for solar total magnetic flux solar irradiance should also show secular trend

45 Reconstruction of open flux back to Be Open solar flux The model and its results were described in detail in Lecture 5 on the solar dynamo Interplanetary field Solanki et al Nature Model also predicts very similar trend for solar total magnetic flux solar irradiance should also show secular trend

46 Solar irradiance since 1610 based on magnetic field reconstruction There is a clear long-term (secular) trend in total solar irradiance from the Maunder minimum till today Estimates of rise in total solar irradiance since Maunder minimum W/m 2 Krivova et al. 2007, 2010

47 Solar irradiance since 1610 based on magnetic field reconstruction There is a clear long-term (secular) trend in total solar irradiance from the Maunder minimum till today Estimates of rise in total solar irradiance since Maunder minimum W/m 2 A secular variation of total solar irradiance > 1.5 W/m 2 cannot be ruled out, but is not likely to be based on variations of solar surface magnetic flux Krivova et al. 2007, 2010

48 Solar Irradiance and Climate

Solar Activity and Earth's Climate

Solar Activity and Earth's Climate Rasmus E. Benestad Solar Activity and Earth's Climate Second Edition Published in association with Springer Praxis ids Publishing Publisl PRAXI Chichester, UK Contents Preface to the second edition Preface

More information

THE SOLAR SYSTEM - EXERCISES 1

THE SOLAR SYSTEM - EXERCISES 1 THE SOLAR SYSTEM - EXERCISES 1 THE SUN AND THE SOLAR SYSTEM Name the planets in their order from the sun. 1 2 3 4 5 6 7 8 The asteroid belt is between and Which planet has the most moons? About how many?

More information

- 1 - Jennifer McClure. To: env.essay@physics.org. From: Jennifer McClure (j.m.mcclure@student.liverpool.ac.uk)

- 1 - Jennifer McClure. To: env.essay@physics.org. From: Jennifer McClure (j.m.mcclure@student.liverpool.ac.uk) To: env.essay@physics.org Jennifer McClure From: Jennifer McClure (j.m.mcclure@student.liverpool.ac.uk) 1 st year Physics (F300), Department of Physics, University of Liverpool. - 1 - The Northern Lights;

More information

Space Weather: An Introduction C. L. Waters. Centre for Space Physics University of Newcastle, Australia

Space Weather: An Introduction C. L. Waters. Centre for Space Physics University of Newcastle, Australia Space Weather: An Introduction C. L. Waters Centre for Space Physics University of Newcastle, Australia 1 Outline Space weather: Conditions on the Sun and in the solar wind, magnetosphere, ionosphere and

More information

Solar Irradiance Variability

Solar Irradiance Variability Solar Radiative Output and its Variability Claus Frölich and Judith Lean Preethi Ganapathy November 22, 2005 Solar Irradiance Variability Historical Investigations Contemporary Investigations Limitations

More information

The Earth's Atmosphere. Layers of the Earth's Atmosphere

The Earth's Atmosphere. Layers of the Earth's Atmosphere The Earth's Atmosphere The atmosphere surrounds Earth and protects us by blocking out dangerous rays from the sun. The atmosphere is a mixture of gases that becomes thinner until it gradually reaches space.

More information

The Earth, Sun, and Moon

The Earth, Sun, and Moon reflect The Sun and Moon are Earth s constant companions. We bask in the Sun s heat and light. It provides Earth s energy, and life could not exist without it. We rely on the Moon to light dark nights.

More information

Atmospheric Layers. Ionosphere. Exosphere. Thermosphere. Mesosphere. Stratosphere. Troposphere. mi (km) above sea level 250 (400) 50 (80) 30 (50)

Atmospheric Layers. Ionosphere. Exosphere. Thermosphere. Mesosphere. Stratosphere. Troposphere. mi (km) above sea level 250 (400) 50 (80) 30 (50) mi (km) above sea level Atmospheric Layers Exosphere 250 (400) Thermosphere Ionosphere 50 (80) Mesosphere Ozone Layer 30 (50) 7 (12) Stratosphere Troposphere Atmospheric Layers Earth s atmosphere is held

More information

Solar Irradiance Variability Observed During Solar Cycle 23

Solar Irradiance Variability Observed During Solar Cycle 23 Solar Irradiance Variability Observed During Solar Cycle 23 Introduction Solar Cycle Results for Climate Change Solar Cycle Results for Space Weather Tom Woods LASP / University

More information

WELCOME to Aurorae In the Solar System. J.E. Klemaszewski

WELCOME to Aurorae In the Solar System. J.E. Klemaszewski WELCOME to Aurorae In the Solar System Aurorae in the Solar System Sponsoring Projects Galileo Europa Mission Jupiter System Data Analysis Program ACRIMSAT Supporting Projects Ulysses Project Outer Planets

More information

Solar Storms and Northern lights - how to predict Space Weather and the Aurora

Solar Storms and Northern lights - how to predict Space Weather and the Aurora Solar Storms and Northern lights - how to predict Space Weather and the Aurora Pål Brekke Norwegian Space Centre/UNIS Pål Brekke torsdag 12. mars 15 Fleet of satellites watching the Sun Stereo SDO SOHO

More information

Name: João Fernando Alves da Silva Class: 7-4 Number: 10

Name: João Fernando Alves da Silva Class: 7-4 Number: 10 Name: João Fernando Alves da Silva Class: 7-4 Number: 10 What is the constitution of the Solar System? The Solar System is constituted not only by planets, which have satellites, but also by thousands

More information

Radiation and plasma/particles. I3/CA Europlanet - EC Contract 001637 - http://europlanet.cesr.fr/

Radiation and plasma/particles. I3/CA Europlanet - EC Contract 001637 - http://europlanet.cesr.fr/ Radiation and plasma/particles X-ray/EUV activity and stellar type and age Early Venus, Earth, Mars, Titan, gas giants, comets Exoplanets [Scalo et al., Astrobiology, submitted, 2006] Hot Jupiter s [Yelle,

More information

Solar Flux and Flux Density. Lecture 3: Global Energy Cycle. Solar Energy Incident On the Earth. Solar Flux Density Reaching Earth

Solar Flux and Flux Density. Lecture 3: Global Energy Cycle. Solar Energy Incident On the Earth. Solar Flux Density Reaching Earth Lecture 3: Global Energy Cycle Solar Flux and Flux Density Planetary energy balance Greenhouse Effect Vertical energy balance Latitudinal energy balance Seasonal and diurnal cycles Solar Luminosity (L)

More information

Satellite Measurements of Solar Spectral Irradiance

Satellite Measurements of Solar Spectral Irradiance Satellite Measurements of Solar Spectral Irradiance LASP University of Colorado tom.woods@lasp.colorado.edu March 2006 1 Talk Outline Motivation for Solar Spectral Irradiance solar energy input climate

More information

The Extreme Solar Storms of October to November 2003

The Extreme Solar Storms of October to November 2003 S.P. Plunkett S.P. Plunkett Space Science Division The Extreme Solar Storms of October to November 2003 AN OVERVIEW OF SOLAR ACTIVITY AND SPACE WEATHER In recent decades, humans have come to rely on space

More information

Science Standard 4 Earth in Space Grade Level Expectations

Science Standard 4 Earth in Space Grade Level Expectations Science Standard 4 Earth in Space Grade Level Expectations Science Standard 4 Earth in Space Our Solar System is a collection of gravitationally interacting bodies that include Earth and the Moon. Universal

More information

Related Standards and Background Information

Related Standards and Background Information Related Standards and Background Information Earth Patterns, Cycles and Changes This strand focuses on student understanding of patterns in nature, natural cycles, and changes that occur both quickly and

More information

U.S. DEPARTMENT OF COMMERCE

U.S. DEPARTMENT OF COMMERCE Space Weather Space Weather Storms from the Sun Storms from the Sun U.S. DEPARTMENT OF COMMERCE National Oceanic and Atmospheric Administration National Weather Service U.S. Department of Commerce National

More information

SPATIAL DISTRIBUTION OF NORTHERN HEMISPHERE WINTER TEMPERATURES OVER THE SOLAR CYCLE DURING THE LAST 130 YEARS

SPATIAL DISTRIBUTION OF NORTHERN HEMISPHERE WINTER TEMPERATURES OVER THE SOLAR CYCLE DURING THE LAST 130 YEARS SPATIAL DISTRIBUTION OF NORTHERN HEMISPHERE WINTER TEMPERATURES OVER THE SOLAR CYCLE DURING THE LAST 130 YEARS Kalevi Mursula, Ville Maliniemi, Timo Asikainen ReSoLVE Centre of Excellence Department of

More information

UNIT V. Earth and Space. Earth and the Solar System

UNIT V. Earth and Space. Earth and the Solar System UNIT V Earth and Space Chapter 9 Earth and the Solar System EARTH AND OTHER PLANETS A solar system contains planets, moons, and other objects that orbit around a star or the star system. The solar system

More information

The Greenhouse Effect. Lan Ma Global Warming: Problems & Solutions 17 September, 2007

The Greenhouse Effect. Lan Ma Global Warming: Problems & Solutions 17 September, 2007 The Greenhouse Effect Lan Ma Global Warming: Problems & Solutions 17 September, 2007 What to cover today: How do we calculate the Earth s surface temperature? What makes a gas a greenhouse gas and how

More information

Solar Ast ro p h y s ics

Solar Ast ro p h y s ics Peter V. Foukal Solar Ast ro p h y s ics Second, Revised Edition WI LEY- VCH WILEY-VCH Verlag Co. KCaA Contents Preface 1 1.1 1.2 1.3 1.4 1.5 1.6 1.7 1.8 1.9 2 2.1 2.1.1 2.1.2 2.2 2.2.1 2.2.2 2.2.3 2.3

More information

California Standards Grades 9 12 Boardworks 2009 Science Contents Standards Mapping

California Standards Grades 9 12 Boardworks 2009 Science Contents Standards Mapping California Standards Grades 912 Boardworks 2009 Science Contents Standards Mapping Earth Sciences Earth s Place in the Universe 1. Astronomy and planetary exploration reveal the solar system s structure,

More information

Studies on the ionospheric region during low solar activity in Brazil

Studies on the ionospheric region during low solar activity in Brazil Studies on the ionospheric region during low solar activity in Brazil Claudia M. N. Candido National Institute for Space Research - INPE Brazil 1 Plasma Bubbles-Spread-F OI 630.0-nm Peak at 250 km - F-layer

More information

Lesson 6: Earth and the Moon

Lesson 6: Earth and the Moon Lesson 6: Earth and the Moon Reading Assignment Chapter 7.1: Overall Structure of Planet Earth Chapter 7.3: Earth s Interior More Precisely 7-2: Radioactive Dating Chapter 7.5: Earth s Magnetosphere Chapter

More information

8.1 Radio Emission from Solar System objects

8.1 Radio Emission from Solar System objects 8.1 Radio Emission from Solar System objects 8.1.1 Moon and Terrestrial planets At visible wavelengths all the emission seen from these objects is due to light reflected from the sun. However at radio

More information

The Celestial Sphere. Questions for Today. The Celestial Sphere 1/18/10

The Celestial Sphere. Questions for Today. The Celestial Sphere 1/18/10 Lecture 3: Constellations and the Distances to the Stars Astro 2010 Prof. Tom Megeath Questions for Today How do the stars move in the sky? What causes the phases of the moon? What causes the seasons?

More information

ULTRALONG SOLAR CYCLE 23 AND POSSIBLE CONSEQUENCES

ULTRALONG SOLAR CYCLE 23 AND POSSIBLE CONSEQUENCES ULTRALONG SOLAR CYCLE 23 AND POSSIBLE CONSEQUENCES By Joseph D Aleo, CCM WHAT ARE SUNSPOTS? In 1610, shortly after viewing the sun with his new telescope, Galileo Galilei made the first European observations

More information

The Earth s Atmosphere

The Earth s Atmosphere THE SUN-EARTH SYSTEM III The Earth s Atmosphere Composition and Distribution of the Atmosphere The composition of the atmosphere and the way its gases interact with electromagnetic radiation determine

More information

Activities of the Japanese Space Weather Forecast Center at Communications Research Laboratory

Activities of the Japanese Space Weather Forecast Center at Communications Research Laboratory J. RADIAT. RES., 43: SUPPL., S53 S57 (2002) Activities of the Japanese Space Weather Forecast Center at Communications Research Laboratory SHINICHI WATARI 1 * and FUMIHIKO TOMITA 1 Space weather / ISES/SEP

More information

Climate Discovery Teacher s Guide

Climate Discovery Teacher s Guide Climate Discovery eacher s Guide Sunspots and Climate Unit:Little Ice Age Lesson: 7 Materials & Preparation ime: Preparation: 10 min eaching: 60 min Materials for the eacher: Overhead projector ransparencies

More information

CHARACTERISTICS OF THE SOLAR SYSTEM

CHARACTERISTICS OF THE SOLAR SYSTEM reflect Our solar system is made up of thousands of objects, at the center of which is a star, the Sun. The objects beyond the Sun include 8 planets, at least 5 dwarf planets, and more than 170 moons.

More information

EASA Safety Information Bulletin

EASA Safety Information Bulletin EASA Safety Information Bulletin SIB No.: 2012-09 Issued: 23 May 2012 Subject: Effects of Space Weather on Aviation Ref. Publication: 1. EU OPS 1.390 Cosmic Radiation; 2. SIB 2012-10 Single Event Effects

More information

ATM S 111, Global Warming: Understanding the Forecast

ATM S 111, Global Warming: Understanding the Forecast ATM S 111, Global Warming: Understanding the Forecast DARGAN M. W. FRIERSON DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 1: OCTOBER 1, 2015 Outline How exactly the Sun heats the Earth How strong? Important concept

More information

Teaching Time: One-to-two 50-minute periods

Teaching Time: One-to-two 50-minute periods Lesson Summary Students create a planet using a computer game and change features of the planet to increase or decrease the planet s temperature. Students will explore some of the same principles scientists

More information

Science Investigations: Investigating Astronomy Teacher s Guide

Science Investigations: Investigating Astronomy Teacher s Guide Teacher s Guide Grade Level: 6 12 Curriculum Focus: Astronomy/Space Duration: 7 segments; 66 minutes Program Description This library of videos contains seven segments on celestial bodies and related science.

More information

Lecture 23: Terrestrial Worlds in Comparison. This lecture compares and contrasts the properties and evolution of the 5 main terrestrial bodies.

Lecture 23: Terrestrial Worlds in Comparison. This lecture compares and contrasts the properties and evolution of the 5 main terrestrial bodies. Lecture 23: Terrestrial Worlds in Comparison Astronomy 141 Winter 2012 This lecture compares and contrasts the properties and evolution of the 5 main terrestrial bodies. The small terrestrial planets have

More information

Counting Sunspots. Parent Prompts: Are there years with lots of sunspots? Are there years with very few sunspots?

Counting Sunspots. Parent Prompts: Are there years with lots of sunspots? Are there years with very few sunspots? Counting are magnetic storms on the Sun these dark areas are a little cooler than the rest of the Sun s atmosphere. They can be easily seen when the Sun s image is projected onto a white surface, using

More information

Perspective and Scale Size in Our Solar System

Perspective and Scale Size in Our Solar System Perspective and Scale Size in Our Solar System Notes Clue Session in Mary Gates RM 242 Mon 6:30 8:00 Read Lang Chpt. 1 Moodle Assignment due Thursdays at 6pm (first one due 1/17) Written Assignments due

More information

The atmospheres of different planets

The atmospheres of different planets The atmospheres of different planets Thomas Baron October 13, 2006 1 Contents 1 Introduction 3 2 The atmosphere of the Earth 3 2.1 Description and Composition.................... 3 2.2 Discussion...............................

More information

Asteroids. Earth. Asteroids. Earth Distance from sun: 149,600,000 kilometers (92,960,000 miles) Diameter: 12,756 kilometers (7,926 miles) dotted line

Asteroids. Earth. Asteroids. Earth Distance from sun: 149,600,000 kilometers (92,960,000 miles) Diameter: 12,756 kilometers (7,926 miles) dotted line Image taken by NASA Asteroids About 6,000 asteroids have been discovered; several hundred more are found each year. There are likely hundreds of thousands more that are too small to be seen from Earth.

More information

FACTS ABOUT CLIMATE CHANGE

FACTS ABOUT CLIMATE CHANGE FACTS ABOUT CLIMATE CHANGE 1. What is climate change? Climate change is a long-term shift in the climate of a specific location, region or planet. The shift is measured by changes in features associated

More information

A: Planets. Q: Which of the following objects would NOT be described as a small body: asteroids, meteoroids, comets, planets?

A: Planets. Q: Which of the following objects would NOT be described as a small body: asteroids, meteoroids, comets, planets? Q: Which of the following objects would NOT be described as a small body: asteroids, meteoroids, comets, planets? A: Planets Q: What can we learn by studying small bodies of the solar system? A: We can

More information

Met Office Space Weather Operations and R&D

Met Office Space Weather Operations and R&D Met Office Space Weather Operations and R&D David Jackson Mark Gibbs, Suzy Bingham, Francois Bocquet, Edmund Henley, Sophie Murray WMO / ISES Meeting, August 9-10 2014, Moscow, Russia Met Office Motivation?

More information

Characteristics of the. thermosphere

Characteristics of the. thermosphere Characteristics of the Atmosphere. If you were lost in the desert, you could survive for a few days without food and water. But you wouldn't last more than five minutes without the ' Objectives Describe

More information

CHAPTER 6 THE TERRESTRIAL PLANETS

CHAPTER 6 THE TERRESTRIAL PLANETS CHAPTER 6 THE TERRESTRIAL PLANETS MULTIPLE CHOICE 1. Which of the following is NOT one of the four stages in the development of a terrestrial planet? 2. That Earth, evidence that Earth differentiated.

More information

The solar wind (in 90 minutes) Mathew Owens

The solar wind (in 90 minutes) Mathew Owens The solar wind (in 90 minutes) Mathew Owens 5 th Sept 2013 STFC Advanced Summer School m.j.owens@reading.ac.uk Overview There s simply too much to cover in 90 minutes Hope to touch on: Formation of the

More information

climate science A SHORT GUIDE TO This is a short summary of a detailed discussion of climate change science.

climate science A SHORT GUIDE TO This is a short summary of a detailed discussion of climate change science. A SHORT GUIDE TO climate science This is a short summary of a detailed discussion of climate change science. For more information and to view the full report, visit royalsociety.org/policy/climate-change

More information

SPACE WEATHER INTERPRETING THE WIND. Petra Vanlommel & Luciano Rodriguez

SPACE WEATHER INTERPRETING THE WIND. Petra Vanlommel & Luciano Rodriguez SPACE WEATHER INTERPRETING THE WIND Petra Vanlommel & Luciano Rodriguez THE SUN LOSES ENERGY Radiation Mass Particles THE SUN LOSES ENERGY PHYSICAL REPHRASING Total Solar Irradiance Solar Wind Fast Particles

More information

STUDY GUIDE: Earth Sun Moon

STUDY GUIDE: Earth Sun Moon The Universe is thought to consist of trillions of galaxies. Our galaxy, the Milky Way, has billions of stars. One of those stars is our Sun. Our solar system consists of the Sun at the center, and all

More information

Progress Towards the Solar Dynamics Observatory

Progress Towards the Solar Dynamics Observatory Progress Towards the Solar Dynamics Observatory Barbara J. Thompson SDO Project Scientist W. Dean Pesnell SDO Assistant Project Scientist Page 1 SDO OVERVIEW Mission Science Objectives The primary goal

More information

DESCRIPTION ACADEMIC STANDARDS INSTRUCTIONAL GOALS VOCABULARY BEFORE SHOWING. Subject Area: Science

DESCRIPTION ACADEMIC STANDARDS INSTRUCTIONAL GOALS VOCABULARY BEFORE SHOWING. Subject Area: Science DESCRIPTION Host Tom Selleck conducts a stellar tour of Jupiter, Saturn, Uranus, Neptune, and Pluto--the outer planets of Earth's solar system. Information from the Voyager space probes plus computer models

More information

The Main Point. Lecture #34: Solar System Origin II. Chemical Condensation ( Lewis ) Model. How did the solar system form? Reading: Chapter 8.

The Main Point. Lecture #34: Solar System Origin II. Chemical Condensation ( Lewis ) Model. How did the solar system form? Reading: Chapter 8. Lecture #34: Solar System Origin II How did the solar system form? Chemical Condensation ("Lewis") Model. Formation of the Terrestrial Planets. Formation of the Giant Planets. Planetary Evolution. Reading:

More information

Fundamentals of Climate Change (PCC 587): Water Vapor

Fundamentals of Climate Change (PCC 587): Water Vapor Fundamentals of Climate Change (PCC 587): Water Vapor DARGAN M. W. FRIERSON UNIVERSITY OF WASHINGTON, DEPARTMENT OF ATMOSPHERIC SCIENCES DAY 2: 9/30/13 Water Water is a remarkable molecule Water vapor

More information

Energy Pathways in Earth s Atmosphere

Energy Pathways in Earth s Atmosphere BRSP - 10 Page 1 Solar radiation reaching Earth s atmosphere includes a wide spectrum of wavelengths. In addition to visible light there is radiation of higher energy and shorter wavelength called ultraviolet

More information

Space Weather: Forecasting & Impacts on Critical Infrastructure

Space Weather: Forecasting & Impacts on Critical Infrastructure Space Weather: Forecasting & Impacts on Critical Infrastructure Dr. Genene Fisher Senior Advisor for Space Weather National Weather Service AMS Washington Forum 12 April 2012 Outline Solar Activity Update

More information

Origins of the Cosmos Summer 2016. Pre-course assessment

Origins of the Cosmos Summer 2016. Pre-course assessment Origins of the Cosmos Summer 2016 Pre-course assessment In order to grant two graduate credits for the workshop, we do require you to spend some hours before arriving at Penn State. We encourage all of

More information

The Sun: Our nearest star

The Sun: Our nearest star The Sun: Our nearest star Property Surface T Central T Luminosity Mass Lifetime (ms) Value 5500K 15x10 6 K 2 x 10 33 ergs 4 x 10 33 grams 10 billion years Solar Structure Build a model and find the central

More information

Solar System Fact Sheet

Solar System Fact Sheet Solar System Fact Sheet (Source: http://solarsystem.nasa.gov; http://solarviews.com) The Solar System Categories Mercury Venus Earth Mars Jupiter Saturn Uranus Neptune Rocky or Gas Rocky Rocky Rocky Rocky

More information

Corso di Fisica Te T cnica Ambientale Solar Radiation

Corso di Fisica Te T cnica Ambientale Solar Radiation Solar Radiation Solar radiation i The Sun The Sun is the primary natural energy source for our planet. It has a diameter D = 1.39x10 6 km and a mass M = 1.989x10 30 kg and it is constituted by 1/3 of He

More information

Multiple Choice Identify the choice that best completes the statement or answers the question.

Multiple Choice Identify the choice that best completes the statement or answers the question. Test 2 f14 Multiple Choice Identify the choice that best completes the statement or answers the question. 1. Carbon cycles through the Earth system. During photosynthesis, carbon is a. released from wood

More information

CHAPTER 5 Lectures 10 & 11 Air Temperature and Air Temperature Cycles

CHAPTER 5 Lectures 10 & 11 Air Temperature and Air Temperature Cycles CHAPTER 5 Lectures 10 & 11 Air Temperature and Air Temperature Cycles I. Air Temperature: Five important factors influence air temperature: A. Insolation B. Latitude C. Surface types D. Coastal vs. interior

More information

FIRST GRADE 1 WEEK LESSON PLANS AND ACTIVITIES

FIRST GRADE 1 WEEK LESSON PLANS AND ACTIVITIES FIRST GRADE 1 WEEK LESSON PLANS AND ACTIVITIES UNIVERSE CYCLE OVERVIEW OF FIRST GRADE UNIVERSE WEEK 1. PRE: Describing the Universe. LAB: Comparing and contrasting bodies that reflect light. POST: Exploring

More information

Study Guide due Friday, 1/29

Study Guide due Friday, 1/29 NAME: Astronomy Study Guide asteroid chromosphere comet corona ellipse Galilean moons VOCABULARY WORDS TO KNOW geocentric system meteor gravity meteorite greenhouse effect meteoroid heliocentric system

More information

Group Leader: Group Members:

Group Leader: Group Members: THE SOLAR SYSTEM PROJECT: TOPIC: THE SUN Required Project Content for an Oral/Poster Presentation on THE SUN - What it s made of - Age and how it formed (provide pictures or diagrams) - What is an AU?

More information

Solar System Overview

Solar System Overview Solar System Overview Planets: Four inner planets, Terrestrial planets Four outer planets, Jovian planets Asteroids: Minor planets (planetesimals) Meteroids: Chucks of rocks (smaller than asteroids) (Mercury,

More information

Assignment 5. Multiple Choice Identify the letter of the choice that best completes the statement or answers the question.

Assignment 5. Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. Assignment 5 Multiple Choice Identify the letter of the choice that best completes the statement or answers the question. 1. What is the single most important reason that astronomers have learned more

More information

Solar atmosphere. Solar activity and solar wind. Reading for this week: Chap. 6.2, 6.3, 6.5, 6.7 Homework #2 (posted on website) due Oct.

Solar atmosphere. Solar activity and solar wind. Reading for this week: Chap. 6.2, 6.3, 6.5, 6.7 Homework #2 (posted on website) due Oct. Solar activity and solar wind Solar atmosphere Reading for this week: Chap. 6.2, 6.3, 6.5, 6.7 Homework #2 (posted on website) due Oct. 17 Photosphere - visible surface of sun. Only ~100 km thick. Features

More information

CHAPTER 3 Heat and energy in the atmosphere

CHAPTER 3 Heat and energy in the atmosphere CHAPTER 3 Heat and energy in the atmosphere In Chapter 2 we examined the nature of energy and its interactions with Earth. Here we concentrate initially on the way in which energy interacts with the atmosphere

More information

Earth Is Not the Center of the Universe

Earth Is Not the Center of the Universe Earth Is Not the Center of the Universe Source: Utah State Office of Education Introduction Have you ever looked up at the night sky and wondered about all the pinpoint lights? People through the ages

More information

We already went through a (small, benign) climate change in The Netherlands

We already went through a (small, benign) climate change in The Netherlands We already went through a (small, benign) climate change in The Netherlands 15-16 October 1987, gusts till 220 km/h, great damage 2004, almost 1400 tornado s December (!!) 2001, Faxai, 879 mbar 27 December

More information

Earth Sciences -- Grades 9, 10, 11, and 12. California State Science Content Standards. Mobile Climate Science Labs

Earth Sciences -- Grades 9, 10, 11, and 12. California State Science Content Standards. Mobile Climate Science Labs Earth Sciences -- Grades 9, 10, 11, and 12 California State Science Content Standards Covered in: Hands-on science labs, demonstrations, & activities. Investigation and Experimentation. Lesson Plans. Presented

More information

Class 2 Solar System Characteristics Formation Exosolar Planets

Class 2 Solar System Characteristics Formation Exosolar Planets Class 1 Introduction, Background History of Modern Astronomy The Night Sky, Eclipses and the Seasons Kepler's Laws Newtonian Gravity General Relativity Matter and Light Telescopes Class 2 Solar System

More information

CHAPTER 2 Energy and Earth

CHAPTER 2 Energy and Earth CHAPTER 2 Energy and Earth This chapter is concerned with the nature of energy and how it interacts with Earth. At this stage we are looking at energy in an abstract form though relate it to how it affect

More information

ATMOSPHERIC STRUCTURE. The vertical distribution of temperature, pressure,

ATMOSPHERIC STRUCTURE. The vertical distribution of temperature, pressure, ATMOSPHERIC STRUCTURE. The vertical distribution of temperature, pressure, density, and composition of the atmosphere constitutes atmospheric structure. These quantities also vary with season and location

More information

Clouds and the Energy Cycle

Clouds and the Energy Cycle August 1999 NF-207 The Earth Science Enterprise Series These articles discuss Earth's many dynamic processes and their interactions Clouds and the Energy Cycle he study of clouds, where they occur, and

More information

astronomy 2008 1. A planet was viewed from Earth for several hours. The diagrams below represent the appearance of the planet at four different times.

astronomy 2008 1. A planet was viewed from Earth for several hours. The diagrams below represent the appearance of the planet at four different times. 1. A planet was viewed from Earth for several hours. The diagrams below represent the appearance of the planet at four different times. 5. If the distance between the Earth and the Sun were increased,

More information

Blackbody radiation. Main Laws. Brightness temperature. 1. Concepts of a blackbody and thermodynamical equilibrium.

Blackbody radiation. Main Laws. Brightness temperature. 1. Concepts of a blackbody and thermodynamical equilibrium. Lecture 4 lackbody radiation. Main Laws. rightness temperature. Objectives: 1. Concepts of a blackbody, thermodynamical equilibrium, and local thermodynamical equilibrium.. Main laws: lackbody emission:

More information

Space Weather Research and Forecasting in CRL, Japan

Space Weather Research and Forecasting in CRL, Japan Space Weather Research and Forecasting in CRL, Japan Maki Akioka Hiraiso Solar Observatory Communications Research Laboratory Contact akioka@crl.go.jp 1 Contents of Presentation 1.Space Weather Observation

More information

Solar Energetic Particles: A Relay Race to Earth By Andrea Karelitz

Solar Energetic Particles: A Relay Race to Earth By Andrea Karelitz Karelitz 1 Solar Energetic Particles: A Relay Race to Earth By Andrea Karelitz Things move fast. If you re feeling daring, take a trip to Brazil and speed down the fastest water slide in the world at 65

More information

Space Weather Prediction Research and Services for China Manned Space Mission

Space Weather Prediction Research and Services for China Manned Space Mission Space Weather Prediction Research and Services for China Manned Space Mission Siqing Liu National Space Science Center, CAS Center for Space Science and Applied Research, CAS Outline I. General information

More information

Mission To Mars! A dialogue activity for upper KS2

Mission To Mars! A dialogue activity for upper KS2 Mission To Mars! A dialogue activity for upper KS2 Teacher s Sheet Mission to Mars: Dialogue activity for upper KS2 Part One: As a class or in groups. pupils read the Fact or Fiction cards. On each card

More information

A long time ago, people looked

A long time ago, people looked Supercool Space Tools! By Linda Hermans-Killam A long time ago, people looked into the dark night sky and wondered about the stars, meteors, comets and planets they saw. The only tools they had to study

More information

ESCI 107/109 The Atmosphere Lesson 2 Solar and Terrestrial Radiation

ESCI 107/109 The Atmosphere Lesson 2 Solar and Terrestrial Radiation ESCI 107/109 The Atmosphere Lesson 2 Solar and Terrestrial Radiation Reading: Meteorology Today, Chapters 2 and 3 EARTH-SUN GEOMETRY The Earth has an elliptical orbit around the sun The average Earth-Sun

More information

ANSWER KEY. Chapter 22. 8. phase 9. spring 10. lunar 11. solar 12. gravity

ANSWER KEY. Chapter 22. 8. phase 9. spring 10. lunar 11. solar 12. gravity Chapter 22 Section 22-1 Review and Reinforce (p. 11) 1. winter 2. At point A the sun would be directly overhead, at point B it would be on the horizon, and at point C it would not be visible because it

More information

Review 1. Multiple Choice Identify the choice that best completes the statement or answers the question.

Review 1. Multiple Choice Identify the choice that best completes the statement or answers the question. Review 1 Multiple Choice Identify the choice that best completes the statement or answers the question. 1. When hydrogen nuclei fuse into helium nuclei a. the nuclei die. c. particles collide. b. energy

More information

2-1-5 Space Radiation Effect on Satellites

2-1-5 Space Radiation Effect on Satellites 2-1-5 Space Radiation Effect on Satellites Solar activity and space environment is considered as fundamental and important factors for space system design and operation. Space and solar radiation is widely

More information

CSSAR Space Science Cooperation

CSSAR Space Science Cooperation CSSAR Space Science Cooperation WANG Shuzhi Center for Space Science and Applied Research Chinese Academy of Science(CSSAR) Table of Contents Brief History of CSSAR International Cooperation CAS Strategic

More information

6 th Grade Science Assessment: Weather & Water Select the best answer on the answer sheet. Please do not make any marks on this test.

6 th Grade Science Assessment: Weather & Water Select the best answer on the answer sheet. Please do not make any marks on this test. Select the be answer on the answer sheet. Please do not make any marks on this te. 1. Weather is be defined as the A. changes that occur in cloud formations from day to day. B. amount of rain or snow that

More information

6. The greatest atmospheric pressure occurs in the 1) troposphere 3) mesosphere 2) stratosphere 4) thermosphere

6. The greatest atmospheric pressure occurs in the 1) troposphere 3) mesosphere 2) stratosphere 4) thermosphere 1. The best evidence of the Earth's nearly spherical shape is obtained through telescopic observations of other planets photographs of the Earth from an orbiting satellite observations of the Sun's altitude

More information

Understanding Solar Variability as Groundwork for Planet Transit Detection

Understanding Solar Variability as Groundwork for Planet Transit Detection Stars as Suns: Activity, Evolution, and Planets IAU Symposium, Vol. 219, 2004 A. K. Dupree and A. O. Benz, Eds. Understanding Solar Variability as Groundwork for Planet Transit Detection Andrey D. Seleznyov,

More information

Study Guide: Solar System

Study Guide: Solar System Study Guide: Solar System 1. How many planets are there in the solar system? 2. What is the correct order of all the planets in the solar system? 3. Where can a comet be located in the solar system? 4.

More information

1.1 A Modern View of the Universe" Our goals for learning: What is our place in the universe?"

1.1 A Modern View of the Universe Our goals for learning: What is our place in the universe? Chapter 1 Our Place in the Universe 1.1 A Modern View of the Universe What is our place in the universe? What is our place in the universe? How did we come to be? How can we know what the universe was

More information

Mars Atmosphere and Volatile EvolutioN (MAVEN) Mission

Mars Atmosphere and Volatile EvolutioN (MAVEN) Mission Mars Atmosphere and Volatile EvolutioN (MAVEN) Mission MAVEN Science Community Workshop December 2, 2012 Particles and Fields Package Solar Energetic Particle Instrument (SEP) Davin Larson and the SEP

More information

KINDERGARTEN 1 WEEK LESSON PLANS AND ACTIVITIES

KINDERGARTEN 1 WEEK LESSON PLANS AND ACTIVITIES KINDERGARTEN 1 WEEK LESSON PLANS AND ACTIVITIES UNIVERSE CYCLE OVERVIEW OF KINDERGARTEN UNIVERSE WEEK 1. PRE: Discovering misconceptions of the Universe. LAB: Comparing size and distances in space. POST:

More information

ESCI-61 Introduction to Photovoltaic Technology. Solar Radiation. Ridha Hamidi, Ph.D.

ESCI-61 Introduction to Photovoltaic Technology. Solar Radiation. Ridha Hamidi, Ph.D. 1 ESCI-61 Introduction to Photovoltaic Technology Solar Radiation Ridha Hamidi, Ph.D. 2 The Sun The Sun is a perpetual source of energy It has produced energy for about 4.6 billions of years, and it is

More information

a) species of plants that require a relatively cool, moist environment tend to grow on poleward-facing slopes.

a) species of plants that require a relatively cool, moist environment tend to grow on poleward-facing slopes. J.D. McAlpine ATMS 611 HMWK #8 a) species of plants that require a relatively cool, moist environment tend to grow on poleward-facing slopes. These sides of the slopes will tend to have less average solar

More information

The Earth System. The geosphere is the solid Earth that includes the continental and oceanic crust as well as the various layers of Earth s interior.

The Earth System. The geosphere is the solid Earth that includes the continental and oceanic crust as well as the various layers of Earth s interior. The Earth System The atmosphere is the gaseous envelope that surrounds Earth. It consists of a mixture of gases composed primarily of nitrogen, oxygen, carbon dioxide, and water vapor. The atmosphere and

More information

Georgia Performance Standards Framework for Science Grade 6. Unit Organizer: UNIVERSE AND SOLAR SYSTEM (Approximate Time 3 Weeks)

Georgia Performance Standards Framework for Science Grade 6. Unit Organizer: UNIVERSE AND SOLAR SYSTEM (Approximate Time 3 Weeks) The following instructional plan is part of a GaDOE collection of Unit Frameworks, Performance Tasks, examples of Student Work, and Teacher Commentary. Many more GaDOE approved instructional plans are

More information