Reminder: All answers MUST GO ON ANSWER SHEET! Answers recorded in the exam booklet will not count.

Similar documents
9/12/2011. Training Course Remote Sensing - Basic Theory & Image Processing Methods September 2011

Inaugural University of Michigan Science Olympiad Tournament

Remote Sensing C. Rank: Points: Science Olympiad North Regional Tournament at the University of Florida. Name(s): Team Name: School Name:

REMOTE SENSING KEY!!

Chapter 1: Introduction

Introduction to RS Lecture 2. NR401 Dr. Avik Bhattacharya 1

REMOTE SENSING TEST!!

Remote Sensing in Meteorology: Satellites and Radar. AT 351 Lab 10 April 2, Remote Sensing

The Atmosphere and Atmospheric Energy Chapter 3 and 4

Section 2: The Atmosphere

Remote Sensing I: Basics

1. The frequency of an electromagnetic wave is proportional to its wavelength. a. directly *b. inversely

11/18/2010. Only part of the spectrum we can see. A rainbow of colors, each corresponding to a different wavelength.

Interpretation of Polar-orbiting Satellite Observations. Atmospheric Instrumentation

Lecture 19: Operational Remote Sensing in Visible, IR, and Microwave Channels

Temperature Scales

Princeton Science Olympiad Invitational Remote Sensing Exam

History of Aerosol Remote Sensing. Mark Smithgall Maria Zatko 597K Spring 2009

Directed Reading. Section: Solar Energy and the Atmosphere RADIATION. identical point on the next wave. waves

9/5/16. Section 3-4: Radiation, Energy, Climate. Common Forms of Energy Transfer in Climate. Electromagnetic radiation.

G109 Midterm Exam (Version A) October 10, 2006 Instructor: Dr C.M. Brown 1. Time allowed 50 mins. Total possible points: 40 number of pages: 5

APPLICATIONS WITH METEOROLOGICAL SATELLITES. W. Paul Menzel. Office of Research and Applications NOAA/NESDIS University of Wisconsin Madison, WI

PRINCIPLES OF REMOTE SENSING. Electromagnetic Energy and Spectral Signatures

What are Aerosols? Suspension of very small solid particles or liquid droplets Radii typically in the range of 10nm to

Remote Sensing. RAHS C Division Invitational

FUNDAMENTALS OF REMOTE SENSING FOR RISKS ASSESSMENT. 1. Introduction

Introduction to Electromagnetic Radiation and Radiative Transfer

Remote Sensing of Snow GEOG 454 / 654

Meteorology Pretest on Chapter 2

1. The most important aspects of the quantum theory.

Electromagnetic Radiation. Physical Principles of Remote Sensing

Preface to the Second Edition. Preface to the First Edition

Reflectivity in Remote Sensing

Satellite Oceanography and Applications 1: Introduction, SST, Ocean color

ElectroMagnetic Radiation (EMR) Lecture 2-3 August 29 and 31, 2005

INTRODUCTION TO MICROWAVE REMOTE SENSING. Dr. A. Bhattacharya

Chapter 02 Energy and Matter in the Atmosphere

Fundamentals of Atmospheric Radiation and its Parameterization

Spectrum of Radiation. Importance of Radiation Transfer. Radiation Intensity and Wavelength. Lecture 3: Atmospheric Radiative Transfer and Climate

Lecture 3: Atmospheric Radiative Transfer and Climate

The Nature of Light. We have a dual model

GRACE Cloudsat CALIPSO Aqua. Metop TRMM TOPEX. Meteor/ SAGE GIFTS NOAA/ POES. Landsat GOES MTSAT. SeaWiFS. Aura. Terra MSG. Jason ICESat SORCE

Lecture 2-07: The greenhouse, global heat engine.

GMES: calibration of remote sensing datasets

1. Weather and climate.

Chapter 14: The Changing Climate

3. Which color of the visible light has the shortest wavelength? A) violet B) green C) yellow D) red

The Atmosphere. Composition of the Atmosphere. Section 2

Chapter 3. Multiple Choice Questions

ASTRO 120 Sample Exam

Chapter 11 Lecture Outline. Heating the Atmosphere

The Electromagnetic Spectrum

Climate and the Atmosphere

PHYS 160 Astronomy Test #2 Fall 2017 Version A

Lecture 5: Greenhouse Effect

(Refer Slide Time: 3:48)

Light. Mike Maloney Physics, SHS

REMOTE SENSING OF THE ATMOSPHERE AND OCEANS

ATS150 Global Climate Change Spring 2019 Candidate Questions for Exam #1

Lecture 2: principles of electromagnetic radiation

Lecture 5: Greenhouse Effect

Planetary Science: Investigations 9-10 I-Check Quiz STUDY GUIDE- ANSWER KEY Name HR Date

National Aeronautics and Space Administration. Earth Day is everyday at NASA. activity booklet

The Atmosphere. Characteristics of the Atmosphere. Section 23.1 Objectives. Chapter 23. Chapter 23 Modern Earth Science. Section 1

Topics: Visible & Infrared Measurement Principal Radiation and the Planck Function Infrared Radiative Transfer Equation

( 1 d 2 ) (Inverse Square law);

Prentice Hall EARTH SCIENCE. Tarbuck Lutgens

8.5 GREENHOUSE EFFECT 8.6 GLOBAL WARMING HW/Study Packet

Electromagnetic Waves

Energy and Radiation. GEOG/ENST 2331 Lecture 3 Ahrens: Chapter 2

SPECTRUM. Dispersion. This phenomenon can be observed in a lab environment using a

Greenhouse Effect. Julia Porter, Celia Hallan, Andrew Vrabel Miles, Gary DeFrance, and Amber Rose

ASTR-101 Section 004 Lecture 9 Rare Earth? John T. McGraw, Professor

ESM 186 Environmental Remote Sensing and ESM 186 Lab Syllabus Winter 2012

Monday, Oct. 2: Clear-sky radiation; solar attenuation, Thermal. nomenclature

Physical Geography 1st Exam

In the space provided, write the letter of the description that best matches the term or phrase. as waves. thermosphere

ATM S 111: Global Warming Solar Radiation. Jennifer Fletcher Day 2: June

wave Electromagnetic Waves

AT 350 EXAM #1 February 21, 2008

CE 59700: Digital Photogrammetric Systems

Atmospheric Lidar The Atmospheric Lidar (ATLID) is a high-spectral resolution lidar and will be the first of its type to be flown in space.

ATMOSPHERE PACKET CHAPTER 22 PAGES Section 1 page 546

Lecture 3: Global Energy Cycle

Mandatory Assignment 2013 INF-GEO4310

Environmental Science Chapter 13 Atmosphere and Climate Change Review

Land Surface Temperature Measurements From the Split Window Channels of the NOAA 7 Advanced Very High Resolution Radiometer John C.

MASSACHUSETTS INSTITUTE OF TECHNOLOGY Department of Physics Problem Solving 10: The Greenhouse Effect. Section Table and Group

Common Elements: Nitrogen, 78%

Earth: the Goldilocks Planet

Lecture 4: Global Energy Balance

Remote Sensing Systems Overview

Lecture 4: Global Energy Balance. Global Energy Balance. Solar Flux and Flux Density. Blackbody Radiation Layer Model.

9/16/08 Tuesday. Chapter 3. Properties of Light. Light the Astronomer s Tool. and sometimes it can be described as a particle!

EUMETSAT STATUS AND PLANS

Topic 5 Practice Test

Grade 8 Science: Unit 3-Optics Chapter 4: Properties of Light

The greenhouse effect

UNIT I EMR AND ITS INTERACTION WITH ATMOSPHERE & EARTH MATERIAL

Lecture Notes Prepared by Mike Foster Spring 2007

Transcription:

Reminder: All answers MUST GO ON ANSWER SHEET! Answers recorded in the exam booklet will not count. 1. Identify the following acronyms; compare these platform types; provide situations where one platform may be more advantageous over another. (6 pts.) SAR LIDAR 2. Many remote sensing studies create land use maps (As in Figure 1 below). How might someone create such a map without physically visiting all the locations on the map? (4 pts.) Figure 1: Land cover map of Australia

3. In figure 2, what is the predominant land cover in 1985? 1988? 1996? 2001? Describe the overall disturbance. (6 pts.) **2 nd Tie Breaker Question Figure 2: Land cover change in the Prince Albert National Park 4. Using remote sensing terminology, what is the difference(s) between the two images in Figure 3? How are these images produced? (6 pts.) Figure 3: Landsat images of Chesapeake Bay. Image A: Image B:

5. Referring to the Basin Characterization Model below, describe how the follow maps are making a case for changes in climate. (4 pts.) 6. Using Figure 4, answer the following questions: If anthropogenic activity disturbs the carbon stored in soils and 550 GtC is released into the atmosphere, calculate the final values for atmosphere, vegetation, and ocean sediments if 25% is absorbed by the atmosphere, 31% by vegetation, and the remainder by ocean sediments. (6 pts.) Figure 4: Global Carbon Cycle (source: Hadley Centre models)

7. Describe the patterns in the AIRS image and provide a possible explanation for the patterns. (4 pts.) 8. Using the figure below, indicate where the following are located: Microwave, Visible Light, Radio, Gamma, X-ray, Ultraviolet, Infrared (1 pt each) 9. Deforestation occurs in many countries around the world at different times therefore it is difficult to detect the ongoing damage. Which of the following remote sensing instruments would be best suited to monitor the deforestation? Explain your answer. Choose one of these instruments (Thermal infrared, Microwave, Radar, Sonar, and Color infrared) (2pts) 10. Describe the relationship between surface air temperature and ground albedo. (2 pts) 11. Write out the full name for the following terms. (1 pt. each) ** 1 st Tie breaker question RADAR SONAR MODIS GOES GRACE SeaWiFS LASER TRMM ETM+ CERES

11. Using the diagram below, answer the following questions: a. What could have caused the relatively low albedo along the mountains? b. What could have caused the relatively high albedo along the coastal plain? c. When did snowmelt start along the mountains? Along the coastal plain? d. Estimate when complete snowmelt occurred. Spatial variations of surface albedo on 23 Apr, 2 May, 24 May, 5 Jun, 11 Jun, and 30 Jul 1997, respectively, on the North Slope of Alaska obtained from the AVHRR Polar Pathfinder data products at the NSIDC.

1. Electromagnetic waves are defined to behave in the same way of which of the following waves? a) Longitudinal waves b) Transverse waves c) Compressional waves d) Sound waves 2. What range of colors are used is for the sensing, representation, and display of images in modern electronic systems and photography? a) Cyan, Magneta, Yellow b) Red, Green, Blue c) Cyan, Green, Yellow d) Red, Green, Yellow 3. Although carbon dioxide is the most important greenhouse gas, methane molecules trap heat with an efficiency that is times larger than that of a molecule of carbon dioxide a) 20 b) 15 c) 10 d) 5 4. The refractive index of the ocean water: a) increases with salinity b) increases with temperature c) decreases with salinity d) decreases with temperature 5. The arrangement of terrain features which provides attributes: the shape, size and texture of objects, is called a) spectral variation b) spatial variation c) temporal variation d) None of these 6. The instruments which provide electromagnetic radiation of specified wave length or a band of wave lengths to illuminate the earth surface, are called a) image sensors b) passive sensors c) active sensors d) none of these 7. If 0 is the angle of scan measured from the nadir, the ground distance swept by the sensor IFOV is proportional to a) sin 2 θ b) cos 2 θ c) sec 2 θ d) tan 2 θ 8. Which one of the following helps to identify the objects on the Earth s surface? a) atmospheric window b) signature c) radiometric error d) None of these 9. The spectral region of the electromagnetic radiation which passes through the atmosphere without much attenuation is known as a) ozone hole b) atmospheric window c) ozone window d) black hole 10. The most widely used antenna in GPS is a) Parabolid antenna b) Microstrip antenna c) Horn antenna d) Slotted antenna

11. Which one of the following parameters is considered to determine the reflectance of a vegetation canopy a) Solar zenith angle b) Azimuth angle c) Number and arrangement of leaves d) All of these 12. The interaction of the electromagnetic radiation produced with a specific wave length to illuminate a target on the terrain for studying its scattered radiance, is called a) passive remote sensing b) active remote sensing c) neutral remote sensing d) None of these 13. In case of reflection and refraction of electromagnetic radiation, a) angle of incidence = angle of refraction b) angle of incidence = angle of reflection c) angle of refraction = sum of the angles of incidence and refraction d) All of the above 14. For interpolation of satellite data used for monitoring dynamic changes that occur on the earth surface, the most suitable orbit for the satellite is a) sun-synchronous orbit b) circular orbit c) near polar orbit d) None of these 15. The ratio of the total solar radiant energy returned by a planetary body to the total radiant energy incident on the body, the called a) reflectance b) reflectance factor c) albedo d) sun glare 16. The reflectance from a surface is called specular reflection if it follows a) Snell s law b) Lambert s cosine law c) Planktan s law d) all of these 17. In sun light, water rich in phytoplankton appears a) red b) green c) brown d) blue 18. What is the most prevalent greenhouse gas in the earth s atmosphere? a. Carbon Dioxide b. Water Vapor c. Methane d. Nitrous Oxide e. Ozone 19. Images sometimes appear slightly to the west of each previous scan due to the eastward rotation of the Earth. This is due to: a. Skew distortion b. Relief displacement c. Tangential scale distortion d. Foreshortening e. None of the above

20. A pulse of light is sent down from a sensor (using lidar) toward Earth. The sensor is orbiting the earth from a distance of approximately 80 km. The pulse is intended to measure the height of a mountain. If the pulse takes.0005 seconds to reach the mountain and get back (to the sensor), how high is the mountain (take the speed of light to be 3 x 105 km/s)? a. 1.8 km b. 2.0 km c. 3.0 km d. 5.0 km 21. What does a dichroic grating do in satellite systems? a. Separates thermal and nonthermal energy b. Separates incident energy into bands 1 and 2 c. Disperses the thermal energy through a prism d. B and C 22. An orthophoto is useful because of its: a. High spatial resolution b. Enhanced topographic relief c. Camera tilt d. Uniform scale e. None of the above 23. An object with an emissivity less than 1 is called a: a. Blackbody b. Graybody c. Selective Radiator d. All of the above e. None of the above 24. Which of the following has the lowest albedo? a) forest b) ocean c) asphalt d) glaciers e) desert 25. The gas that shows the most variation from place to place and from time to time in the lower atmosphere a) ozone (O3) b) carbon dioxide (CO2) c) water vapor (H2O) d) methane (CH4) e) argon (Ar) 26. In the atmosphere, tiny solid or liquid suspended particles of various composition are called a) aerosols b) carcinogens c) greenhouse gases d) microbes 27. The combined albedo of the earth and the atmosphere is approximately a) 4% b) 10% c) 30% d) 50% e) 90% 28. The albedo of the earth's surface is only about 4%, yet the combined albedo of the earth and the atmosphere is higher. Which set of conditions below best explains why this is so? a) high albedo of clouds, low albedo of water b) high albedo of clouds, high albedo of water c) low albedo of clouds, low albedo of water d) low albedo of clouds, high albedo of water