Earth System

Total Page：16

File Type：pdf, Size：1020Kb

Name: Date: Deserts Quiz Class: 1. What do all deserts have in common? 6. What can you infer about penguins from the a. They're all very hot. information presented in the movie? b. They all lack fertile soil. a. Their diet consists mainly of fish. c. They are all very flat. b. They live in the coldest parts of Antarctica. d. They are all completely empty of human life. c. They live alone, and not in groups. d. They are not true birds. 2. A desert's climate is mostly determined by its: a. Latitude 7. Compared to the Sahara Desert, the Gobi Desert is: b. Size a. Wetter c. Population b. Hotter d. Vegetation c. Cooler d. Drier 3. Which two factors keep the Sahara Desert hot? 8. Antelope squirrels and scorpions are nocturnal desert animals. What can you conclude about them from this fact? a. They live in temperate deserts a. Distance from the ocean and very long summer days b. They live in cold deserts b. Volcanic activity and low-pressure air masses c. They live in the parts of deserts nearest to the ocean c. High-pressure air masses and direct sunlight d. They live in hot deserts d. Heat-absorbing soil and abundant hot springs 9. Most animals in hot deserts can't: 4. Which continent is virtually all desert? a. Drink liquid water a. Africa b. Sweat b. South America c. Sleep c. Asia d. Walk d. Antarctica 10. The roots of cactuses: 5. In which region can the air hold the most moisture? a. The North and South Poles b. The area around the equator c. Temperate zones, like most of the United States d. The tundra, which exists in northern Canada and a. Are shallow, but cover a large area. Russia b. Penetrate deep below the surface of the earth. c. Are extremely thick. d. Expel water into the ground. © 1999 - 2019 BrainPOP. All rights reserved..

Copy Link

Recommended publications

M O J a V E D E S E R T I S S U E S a Secondary
MOJAVE DESERT ISSUES A Secondary School Curriculum Bruce W. Bridenbecker & Darleen K. Stoner, Ph.D. Research Assistant Gail Uchwat Mojave Desert Issues was funded with a grant from the National Park �� Foundation. Parks as Classrooms is the educational program of the National �� Park Service in partnership with the National Park Foundation. Design by Amy Yee and Sandra Kaye Published in 1999 and printed on recycled paper ii iii ACKNOWLEDGMENTS Thanks to the following people for their contribution to this work: Elayn Briggs, Bureau of Land Management Caryn Davidson, National Park Service Larry Ellis, Banning High School Lorenza Fong, National Park Service Veronica Fortun, Bureau of Land Management Corky Hays, National Park Service Lorna Lange-Daggs, National Park Service Dave Martell, Pinon Mesa Middle School David Moore, National Park Service Ruby Newton, National Park Service Carol Peterson, National Park Service Pete Ricards, Twentynine Palms Highschool Kay Rohde, National Park Service Dennis Schramm, National Park Service Jo Simpson, Bureau of Land Management Kirsten Talken, National Park Service Cindy Zacks, Yucca Valley Highschool Joe Zarki, National Park Service The following specialists provided information: John Anderson, California Department of Fish & Game Dave Bieri, National Park Service �� John Crossman, California Department of Parks and Recreation �� Don Fife, American Land Holders Association Dana Harper, National Park Service Judy Hohman, U. S. Fish and Wildlife Service Becky Miller, California
[Show full text]
Climate Change Vulnerability and Adaptation Strategies for Natural Communities Piloting Methods in the Mojave and Sonoran Deserts
Climate Change Vulnerability and Adaptation Strategies for Natural Communities Piloting methods in the Mojave and Sonoran deserts September 2012 i Prepared by Patrick J. Comer, Chief Ecologist, NatureServe Bruce Young, Director of Species Science, NatureServe Keith Schulz, Regional Vegetation Ecologist, NatureServe Gwen Kittel, Regional Riparian Ecologist, NatureServe Bob Unnasch, Terrestrial Ecologist, Sound Science David Braun, Aquatic Ecologist/Biohydrologist, Sound Science Geoff Hammerson, Research Zoologist, NatureServe Lindsey Smart, Ecologist/Spatial Analyst, NatureServe Healy Hamilton, Climate Scientist/Ecologist, Stephanie Auer, Climate Scientist/Spatial Analyst Regan Smyth, Landscape Ecologist/Spatial Analyst, NatureServe Jon Hak, Ecologist/Spatial Modeler, NatureServe Citation: Comer, P. J., B. Young, K. Schulz, G. Kittel, B. Unnasch, D. Braun, G. Hammerson, L. Smart, H. Hamilton, S. Auer, R. Smyth, and J. Hak.. 2012. Climate Change Vulnerability and Adaptation Strategies for Natural Communities: Piloting methods in the Mojave and Sonoran deserts. Report to the U.S. Fish and Wildlife Service. NatureServe, Arlington, VA. ii Table of Contents Executive Summary ...................................................................................................................................... 1 Introduction and Project Overview ............................................................................................................... 4 Defining Climate-Change Vulnerability and Adaptation Strategies ........................................................
[Show full text]
Biome (Desert)- Climate Affecting Soil And
With reference to one biome that you have studied, account for the type of climate experienced in this biome and explain how this climate impacts on soils and vegetation within the biome. (80 marks) Marking Scheme: Number of aspects discussed: 3 @ 20 marks each 4 @ 15 marks each For each aspect: Identifying aspect 4 marks 3 marks Discussion 8 x SRPs 6 x SRPs Overall Coherence 20 marks graded* 20 marks graded* In this answer, I choose 3 aspects to discuss (1. Climate, 2. Climate’s impact on soil and, 3. Climate’s impact on vegetation). Overall coherence means how well your answer is structured (Introduction, main section, conclusion – well-structured and coherent) and do you keep to the point/ answer the question directly. Introduction: In this answer I am going to discuss the type of climate experienced in the hot desert biome and how this climate impacts on soils and vegetation within this biome. Biomes are classified according to the predominant vegetation and characterized by adaptations of organisms to that particular environment. They are a large geographical area controlled by climate. Therefore the climate of a particular region will affect what type of soil is formed in that biome as well as what types of plants (flora) grow there. The hot desert that I have studied is the North American Desert Biome. Body of Topic: A desert biome can be defined as an arid region that is characterised by little or no rainfall, in which vegetation is scarce or absent, unless it has specially adapted. As a result of its location, between 15º and 30º north of the Equator, the climate of the hot desert biome is hot and dry.
[Show full text]
Energy from the Desert
SUMMARY Energy from the Desert Feasibility of Very Large Scale Photovoltaic Power Generation (VLS-PV) Systems EDITOR Kosuke Kurokawa Energy from the Desert SUMMARY Energy from the Desert Feasibility of Very Large Scale Photovoltaic Power Generation (VLS-PV) Systems EDITOR Kosuke Kurokawa PART THREE: SCENARIO STUDIES AND RECOMMENDATIONS Published by James & James (Science Publishers) Ltd 8–12 Camden High Street, London, NW1 0JH, UK © Photovoltaic Power Systems Executive Committee of the International Energy Agency The moral right of the author has been asserted. All rights reserved. No part of this book may be reproduced in any form or by any means electronic or mechanical, including photocopying, recording or by any information storage and retrieval system without permission in writing from the copyright holder and the publisher. A catalogue record for this book is available from the British Library. Printed in Hong Kong by H&Y Printing Ltd Cover image: Horizon Stock Images / Michael Simmons Neither the authors nor the publisher make any warranty or representation, expressed or implied, with respect to the information contained in this publication, or assume any liability with respect to the use of, or damages resulting from, this information. Please note: in this publication a comma has been used as a decimal point, according to the ISO standard adopted by the International Energy Agency. CHAPTER ELEVEN: CONCLUSIONS OF PART 1 AND PART 2 Contents Foreword vi Preface vii Task VIII Participants viii COMPREHENSIVE SUMMARY Objective 1 Background and concept of VLS-PV 1 VLS-PV case studies 1 Scenario studies 2 Understandings 2 R ecommendations 2 EXECUTIVE SUMMARY A.
[Show full text]
The Mediterranean Climate: an Overview of the Main Characteristics and Issues
Introduction The Mediterranean Climate: An Overview of the Main Characteristics and Issues P. Lionello,1 P. Malanotte-Rizzoli,2 R. Boscolo,3 P. Alpert,4 V. Artale,5 L. Li,6 J. Luterbacher,7 W. May,10 R. Trigo,8 M. Tsimplis,9 U. Ulbrich11 and E. Xoplaki7 1Department of Material Sciences, University of Lecce, Italy, [email protected] 2Massachusetts Institute of Technology, USA, [email protected] 3ICPO, UK and Spain, [email protected] 4Tel Aviv University, Israel, [email protected] 5ENEA, Roma, Italy, [email protected] 6Laboratory of Dynamical Meteorology CNRS, Paris, France, [email protected] 7Institute of Geography and NCCR Climate, University of Bern and NCCR Climate, Switzerland, [email protected], [email protected] 8University of Lisbon, Portugal, [email protected] 9National Oceanography Centre, Southampton, UK, [email protected] 10Danish Meteorological Institute, Copenhagen, Denmark, [email protected] 11Freie Universita¨t Berlin, Germany, [email protected] 1. The Mediterranean Region: Climate and Characteristics The Mediterranean Region has many morphologic, geographical, historical and societal characteristics, which make its climate scientifically interesting. The purpose of this introduction is to summarize them and to introduce the material extensively discussed in the succeeding chapters of this book. The connotation of ‘‘Mediterranean climate’’ is included in the qualitative classification of the different types of climate on Earth (e.g. Ko¨ppen, 1936) and it has been used to define the climate of other (generally smaller) regions besides that of the Mediterranean region itself. The concept of ‘‘Mediterranean’’ climate is characterized by mild wet winters and warm to hot, dry summers and may occur on the west side of continents between about 30 and 40 latitude.
[Show full text]
Outdoor Comfort: Hot Desert and Cold Winter Cities
Arch. &Comport. I Arch. & Behav., Vol. 10, no 1, p. 73 - 94 73 Outdoor Comfort : Hot Desert and Cold Winter Cities Madis Pihlak Landscape Architecture Program Department of Horticulture University of Maryland College Park, MD 20742-5611 U.S.A. Summary Cities of extreme climate highlight the need for climate sensitive urban design at the site design scale. Relatively inexpensive energy costs have allowed cities as different climatically as Edmonton, Alberta and Phoenix, Arizona to develop more or less in the same manner. Both cities ignore their unique climate and thus any potential to capitalize on their unique characteristics. Both the Sonoran Desert and the high Canadian Prairie are starkly beautiful natural places. By using site design principles which maximize the positive aspects and minimize the negative aspects of each climate type, both cities could develop as uniquely beautiful and comfortable urban places. Most of the literature to date has focused on interior architectural issues of energy conservation or interior comfort. Some urban planning work has focused on the general issue of climate sensitive urban design. There is need for further research with extreme climate cities to develop site level outdoor design principles which will improve everyday comfort within hot desert and cold winter cities. Resume Les villes jouissant d'un climat extreme mettent en Cvidence l'importance d'une planification qui tiendrait compte de cet aspect. Le cofit relativement bas de l'tnergie a permis B des villes aussi diffkrentes sur le plan du climat qu'Edmonton, Alberta, et Phoenix, Arizona, de se dtvelopper de manikre assez semblable. Ces deux villes ne tiennent pas compte du fait qu'elles jouissent d'un climat unique et nCgligent donc toute possibilitC de profiter de cet aspect.
[Show full text]
Precipitation History and Ecosystem Response to Multidecadal Precipitation Variability in the Mojave Desert Region, 1893–2001
ARTICLE IN PRESS Journal of Arid Environments Journal of Arid Environments 67 (2006) 13–34 www.elsevier.com/locate/jaridenv Precipitation history and ecosystem response to multidecadal precipitation variability in the Mojave Desert region, 1893–2001 R. HerefordÃ,1, R.H. Webb, C.I. Longpre´ US Geological Survey, 2255 North Gemini Drive, Flagstaff, Arizona 86001, USA; 520 North Park Avenue Tucson, AZ 85719, USA Abstract Precipitation varied substantially in the Mojave Desert through the 20th century in a manner broadly similar to the other warm North American deserts. Episodes of drought and prolonged dry conditions (1893–1904, ca. 1942–1975, and 1999-present) alternated with relatively wet periods (1905–ca. 1941 and ca. 1976–1998), probably because of global-scale climate fluctuations. These are the El Ninõ-Southern Oscillation that affects interannual climate and the Pacific Decadal Oscillation that evidently causes decadal-scale variability such as prolonged dry and wet episodes. Studies done in the late 20th century demonstrate that precipitation fluctuations affected populations of perennial vegetation, annuals, and small herbivores. Landscape rephotography reveals that several species, particularly creosote bush, increased in size and density during the ca. 1976–1998 wet period. A brief, intense drought from 1989 to 1991 and the ongoing drought caused widespread mortality of certain species; for example, chenopods and perennial grasses suffered up to 100% mortality. Drought pruning, the shedding of above-ground biomass to reduce carbon allocation, increased substantially during drought. Overall, drought had the greatest influence on the Mojave Desert ecosystem. r 2006 Published by Elsevier Ltd. Keywords: Mojave desert; Precipitation variability; ENSO; PDO; Desert ecosystem ÃCorresponding author.
[Show full text]
Hydrological and Climatic Changes in Deserts of China Since the Late Pleistocene
Quaternary Research 73 (2010) 1–9 Contents lists available at ScienceDirect Quaternary Research journal homepage: www.elsevier.com/locate/yqres Hydrological and climatic changes in deserts of China since the late Pleistocene Xiaoping Yang a,⁎, Louis A. Scuderi b a Key Laboratory of Cenozoic Geology and Environment, Institute of Geology and Geophysics, Chinese Academy of Sciences, P.O. Box 9825, Beijing 100029, China b Department of Earth and Planetary Sciences, University of New Mexico, MSC032040 Albuquerque, NM 87131, USA article info abstract Article history: Large areas in western China were wetlands or less arid between 40 and 30 ka, corresponding to the Received 6 April 2009 “Greatest Lake Period” on the adjacent Tibetan Plateau. During the last glacial maximum, some of these Available online 17 November 2009 western Chinese deserts again experienced wetter conditions; however, at the same time the sandy lands in the eastern Chinese desert belt experienced an activation of aeolian dunes. While interpretations of the mid- Keywords: Holocene environment in the deserts of China are controversial, it is quite likely that it was more humid not Dune only in the eastern areas inﬂuenced by monsoon climate systems but also in the western deserts where Desert Lacustrine record moisture is currently associated with westerlies. Evaluation of lacustrine records in the lakes recharged by Late Quaternary dryland rivers and the complex interactions of these systems, as well as other paleoenvironmental proxies Holocene such as the Artemisia/Chenopodiaceae ratio, should be interpreted with greater caution. Facing the China highlighted uncertainties in our understanding of climate changes in Chinese deserts, it is hoped that this special issue will improve our knowledge considerably.
[Show full text]
World Deserts
HISTORY AND GEOGRAPHY World Deserts Reader Frog in the Australian Outback Joshua tree in the Mojave Desert South American sheepherder Camel train across the Sahara Desert THIS BOOK IS THE PROPERTY OF: STATE Book No. PROVINCE Enter information COUNTY in spaces to the left as PARISH instructed. SCHOOL DISTRICT OTHER CONDITION Year ISSUED TO Used ISSUED RETURNED PUPILS to whom this textbook is issued must not write on any page or mark any part of it in any way, consumable textbooks excepted. 1. Teachers should see that the pupil’s name is clearly written in ink in the spaces above in every book issued. 2. The following terms should be used in recording the condition of the book: New; Good; Fair; Poor; Bad. World Deserts Reader Creative Commons Licensing This work is licensed under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License. You are free: to Share—to copy, distribute, and transmit the work to Remix—to adapt the work Under the following conditions: Attribution—You must attribute the work in the following manner: This work is based on an original work of the Core Knowledge® Foundation (www.coreknowledge.org) made available through licensing under a Creative Commons Attribution-NonCommercial-ShareAlike 4.0 International License. This does not in any way imply that the Core Knowledge Foundation endorses this work. Noncommercial—You may not use this work for commercial purposes. Share Alike—If you alter, transform, or build upon this work, you may distribute the resulting work only under the same or similar license to this one. With the understanding that: For any reuse or distribution, you must make clear to others the license terms of this work.
[Show full text]
For Creative Minds
The For Creative Minds educational section may be photocopied or printed from our website by the owner of this book for educational, non-commercial uses. Sheet music for the songs, cross-curricular teaching activities, interactive quizzes, and more are availableFor online. Creative Go to www.ArbordalePublishing.com Minds and click on the book’s cover to explore all the links. Some deserts are hot, and some are cold, but the one thing that all deserts have in common is that they are dry. OnThe average, Desert a desert Habitat gets less than 10 to 12 inches (25- 30 cm) of rain a year. Some do not even get that much. The driest place on Earth, the Atacama Desert in South America has areas that haven’t seen any rain in 400 years! Hot (tropical or subtropical) deserts are warm throughout the year, but very hot in the summer. Temperatures drop at night to cool or cold. Rain comes in short bursts any time of the year and may even evaporate before it hits the ground. There Polar deserts have long, cold winters and can have are long, dry periods in between rain showers. The snow- or ice-covered ground. Chihuahan, Sonoran, and Mojave Deserts in Mexico Antarctica and parts of Arctic and the American Southwest are hot deserts. The Europe and North America Sahara and Kalahari Deserts in Africa are also hot. are polar deserts. Coastal deserts are found along Cold winter deserts (also called semi-arid continental coasts and have salty deserts) have cold winters with some soils or sand.
[Show full text]
Agriculture Project in India: Hypothetical Agriculture Project for India1
Climate and Disaster Risk Screening Report for Agriculture Project in India: Hypothetical Agriculture Project for India1 1 This is the output report from applying the World Bank Group's Climate and Disaster Risk Screening Project Level Tool. The findings, interpretations, and conclusions expressed from applying this tool are those of the individual that applied the tool and should be in no way attributed to the World Bank, to its affiliated institutions, to the Executive Directors of The World Bank or the governments they represent. The World Bank does not guarantee the accuracy of the information included in the screening and this associated output report and accepts no liability for any consequence of its use. 1/11 1. Introduction The project level Climate and Disaster Risks Screening Tool provides due diligence on climate and disaster risks at an early concept stage. The tool uses an exposure - sensitivity - adaptive capacity framework to consider and characterize risks from climate and geophysical hazards, based on key components of a project and its broader development context (Annex 1). The tool helps inform consultation, dialogue, and further work to be done in the course of project design. The results of applying the project level tool to screen for climate and disaster risks for "Hypothetical Agriculture Project" in India are summarized below. 2/11 2. Climate and Disaster Risk Screening Results Summary 2.1 Project Information Summary Table 1 below provides key project information. Table 1: Project Information Project Information
[Show full text]
Hazards and Human-Environment Systems in the Gobi Desert, Asia Troy Sternberg* School of Geography, South Parks Road, Oxford, OX1 3QY, UK
aphy & N r at og u e ra G l Sternberg, J Geogr Nat Disast 2013, 3:1 f D o i s l a Journal of a s DOI: 10.4172/2167-0587.1000106 n t r e u r s o J ISSN: 2167-0587 Geography & Natural Disasters ResearchResearch Article Article OpenOpen Access Access Hazards and Human-Environment Systems in the Gobi Desert, Asia Troy Sternberg* School of Geography, South Parks Road, Oxford, OX1 3QY, UK Abstract Climate hazards are a significant challenge for human and environmental systems in the Gobi Desert, Asia. Drought and extreme cold events frame ecological productivity and livelihood viability in the region. To investigate hazard impact this study uses the Standard Precipitation Index (SPI) to identify drought in southern Mongolia from 1970-2006. It then examines the relationship of drought with climate factors and its interaction with local human and livestock populations. Stressing the extreme winter disasters of 1999-2001 the study then evaluates the resilience of human-environment systems in the Gobi .Results indicate that drought is recurrent in the region, reaching extreme intensity most recently in 2005-2006. In contrast to the prevailing concept of drought impacting severe winters, the study did not find a connection between the two natural hazards. The principal long-term correlation of drought is with human population rather than natural factors, extreme conditions, or livestock numbers. Findings reflect human and landscape resilience when encountering drought and extreme winter conditions. Keywords: Drought; Dzud; Hazard; Mongolia; Standard in isolation from herder action and impact [15,16]. This is essential precipitation index when considering how subtle fluctuations in natural conditions or human action can impact livelihood and grassland productivity.
[Show full text]