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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. -
Spatially-Explicit Modeling of Modern and Pleistocene Runoff and Lake Extent in the Great Basin Region, Western United States
Spatially-explicit modeling of modern and Pleistocene runoff and lake extent in the Great Basin region, western United States Yo Matsubara1 Alan D. Howard1 1Department of Environmental Sciences University of Virginia P.O. Box 400123 Charlottesville, VA 22904-4123 Abstract A spatially-explicit hydrological model balancing yearly precipitation and evaporation is applied to the Great Basin Region of the southwestern United States to predict runoff magnitude and lake distribution during present and Pleistocene climatic conditions. The model iteratively routes runoff through, and evaporation from, depressions to find a steady state solution. The model is calibrated with spatially-explicit annual precipitation estimates and compiled data on pan evaporation, mean annual temperature, and total yearly runoff from stations. The predicted lake distribution provides a close match to present-day lakes. For the last glacial maximum the sizes of lakes Bonneville and Lahontan were well predicted by linear combinations of decrease in mean annual temperature from 0 to 6 °C and increases in precipitation from 0.8 to 1.9 times modern values. Estimated runoff depths were about 1.2 to 4.0 times the present values and yearly evaporation about 0.3 to 1 times modern values. 2 1. Introduction The Great Basin of the southwestern United States in the Basin and Range physiographic province contains enclosed basins featuring perennial and ephemeral lakes, playas and salt pans (Fig. 1). The Great Basin consists of the entire state of Nevada, western Utah, and portions of California, Idaho, Oregon, and Wyoming. At present it supports an extremely dry, desert environment; however, about 40 lakes (some reaching the size of present day Great Lakes) episodically occupied the Great Basin, most recently during the last glacial maximum (LGM) [Snyder and Langbein, 1962; Hostetler et al., 1994; Madsen et al., 2001]. -
North American Deserts Chihuahuan - Great Basin Desert - Sonoran – Mojave
North American Deserts Chihuahuan - Great Basin Desert - Sonoran – Mojave http://www.desertusa.com/desert.html In most modern classifications, the deserts of the United States and northern Mexico are grouped into four distinct categories. These distinctions are made on the basis of floristic composition and distribution -- the species of plants growing in a particular desert region. Plant communities, in turn, are determined by the geologic history of a region, the soil and mineral conditions, the elevation and the patterns of precipitation. Three of these deserts -- the Chihuahuan, the Sonoran and the Mojave -- are called "hot deserts," because of their high temperatures during the long summer and because the evolutionary affinities of their plant life are largely with the subtropical plant communities to the south. The Great Basin Desert is called a "cold desert" because it is generally cooler and its dominant plant life is not subtropical in origin. Chihuahuan Desert: A small area of southeastern New Mexico and extreme western Texas, extending south into a vast area of Mexico. Great Basin Desert: The northern three-quarters of Nevada, western and southern Utah, to the southern third of Idaho and the southeastern corner of Oregon. According to some, it also includes small portions of western Colorado and southwestern Wyoming. Bordered on the south by the Mojave and Sonoran Deserts. Mojave Desert: A portion of southern Nevada, extreme southwestern Utah and of eastern California, north of the Sonoran Desert. Sonoran Desert: A relatively small region of extreme south-central California and most of the southern half of Arizona, east to almost the New Mexico line. -
Central Basin and Range Ecoregion
Status and Trends of Land Change in the Western United States—1973 to 2000 Edited by Benjamin M. Sleeter, Tamara S. Wilson, and William Acevedo U.S. Geological Survey Professional Paper 1794–A, 2012 Chapter 20 Central Basin and Range Ecoregion By Christopher E. Soulard This chapter has been modified from original material Wasatch and Uinta Mountains Ecoregion, on the north by the published in Soulard (2006), entitled “Land-cover trends of Northern Basin and Range and the Snake River Basin Ecore- the Central Basin and Range Ecoregion” (U.S. Geological gions, and on the south by the Mojave Basin and Range and Survey Scientific Investigations Report 2006–5288). the Colorado Plateaus Ecoregions (fig. 1). Most of the Central Basin and Range Ecoregion is located in Nevada (65.4 percent) and Utah (25.1 percent), but small segments are also located Ecoregion Description in Idaho (5.6 percent), California (3.7 percent), and Oregon (0.2 percent). Basin-and-range topography characterizes the The Central Basin and Range Ecoregion (Omernik, 1987; Central Basin and Range Ecoregion: wide desert valleys are U.S. Environmental Protection Agency, 1997) encompasses bordered by parallel mountain ranges generally oriented north- approximately 343,169 km² (132,498 mi2) of land bordered on south. There are more than 33 peaks within the Central Basin the west by the Sierra Nevada Ecoregion, on the east by the and Range Ecoregion that have summits higher than 3,000 m 120° 118° 116° 114° 112° EXPLANATION 42° Land-use/land-cover class Northern Basin ECSF Snake River Basin Water Forest and Range Developed Grassland/Shrubland Transitional Agriculture Mining Wetland MRK Barren Ice/Snow Ecoregion boundary 40° WB Sample block (10 x 10 km) 0 50 100 150 MILES 0 50 100 150 KILOMETERS WUM OREGON IDAHO bo um ld 38° H t R iver Ogden Sparks Reno 80 Sierra Truckee River Lockwood GREAT Tooele Nevada Salt Carson River Lake Walker RiverBASIN City Walker Lake SIERRA NEVADA CCV Mojave DESERT UTAH Basin and Range Colorado NEVADA 36° SCCCOW Plateaus SCM ANMP CALIFORNIA Figure 1. -
Algae and Invertebrates of a Great Basin Desert Hot Lake: a Description of the Borax Lake Ecosystem of Southeastern Oregon
Conference Proceedings. Spring-fed Wetlands: Important Scientific and Cultural Resources of the Intermountain Region, 2002. http://www.wetlands.dri.edu Algae and Invertebrates of a Great Basin Desert Hot Lake: A description of the Borax Lake ecosystem of southeastern Oregon Joseph Furnish Pacific Southwest Region 5, U.S. Department of Agriculture, Forest Service, Vallejo, CA [email protected] James McIver Pacific Northwest Research Station, U.S. Department of Agriculture, Forest Service, LaGrande, OR Mark Teiser Department of Oceanography, Oregon State University, Corvallis, OR Abstract Introduction As part of the recovery plan for the Borax Lake is a geothermally heated endangered chub Gila boraxobius (Cyprinidae), alkaline lake in southeastern Oregon. It a description of algal and invertebrate represents one of the only permanent water populations was undertaken at Borax Lake in sources in the Alvord Desert, which receives 1991 and 1992. Borax Lake, the only known less than 20 cm of rain annually (Green 1978; habitat for G. boraxobius, is a warm, alkaline Cobb et al. 1981). Borax Lake is the only known water body approximately 10 hectares in size habitat for Gila boraxobius, the Borax Lake with an average surface water temperature of chub, a cyprinid fish recognized as a new 30°C. Periphyton algae were surveyed by species in 1980. The chub was listed as scraping substrates and incubating microscope endangered under the Endangered Species Act slides in the water column. Invertebrates were in 1982 because it was believed that geothermal- collected using dip nets, pitfall traps and Ekman energy test-well drilling activities near Borax dredges. The aufwuchs community was Lake might jeopardize its habitat by altering the composed of 23 species and was dominated by flow or temperature of water in the lake. -
Sensitivity of the Colorado Plateau to Change: Climate, Ecosystems, and Society
Copyright © 1969 by the author(s). Published here under license by the Resilience Alliance. Schwinning, S., J. Belnap, D. R. Bowling, and J. R. Ehleringer. 2008. Sensitivity of the Colorado Plateau to change: climate, ecosystems, and society. Ecology and Society XX(YY): ZZ. [online] URL: http://www.ec ologyandsociety.org/volXX/issYY/artZZ/ Synthesis Sensitivity of the Colorado Plateau to Change: Climate, Ecosystems, and Society Susan Schwinning, Jayne Belnap 1, David R. Bowling 2, and James R. Ehleringer 2 ABSTRACT. The Colorado Plateau is located in the interior, dry end of two moisture trajectories coming from opposite directions, which have made this region a target for unusual climate fluctuations. A multi- decadal drought event some 850 years ago may have eliminated maize cultivation by the first human settlers of the Colorado Plateau, the Fremont and Anasazi people, and contributed to the abandonment of their settlements. Even today, ranching and farming are vulnerable to drought and struggle to persist. The recent use of the Colorado Plateau primarily as rangeland has made this region less tolerant to drought due to unprecedented levels of surface disturbances that destroy biological crusts, reduce soil carbon and nitrogen stocks, and increase rates of soil erosion. The most recent drought of 2002 demonstrated the vulnerability of the Colorado Plateau in its currently depleted state and the associated costs to the local economies. New climate predictions for the southwestern United States include the possibility of a long-term shift to warmer, more arid conditions, punctuated by megadroughts not seen since medieval times. It remains to be seen whether the present-day extractive industries, aided by external subsidies, can persist in a climate regime that apparently exceeded the adaptive capacities of the Colorado Plateau’s prehistoric agriculturalists. -
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. -
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. -
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. -
Earth System
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. -
Contraction of the Gobi Desert, 2000–2012
Remote Sens. 2015, 7, 1346-1358; doi:10.3390/rs70201346 OPEN ACCESS remote sensing ISSN 2072-4292 www.mdpi.com/journal/remotesensing Article Contraction of the Gobi Desert, 2000–2012 Troy Sternberg *, Henri Rueff and Nick Middleton School of Geography, University of Oxford, South Parks Road, Oxford OX1 3QY, UK; E-Mails: [email protected] (H.R.); [email protected] (N.M.) * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +44-186-5285-070. Academic Editors: Arnon Karnieli and Prasad S. Thenkabail Received: 5 September 2014 / Accepted: 21 January 2015 / Published: 26 January 2015 Abstract: Deserts are critical environments because they cover 41% of the world’s land surface and are home to 2 billion residents. As highly dynamic biomes desert expansion and contraction is influenced by climate and anthropogenic factors with variability being a key part of the desertification debate across dryland regions. Evaluating a major world desert, the Gobi in East Asia, with high resolution satellite data and the meteorologically-derived Aridity Index from 2000 to 2012 identified a recent contraction of the Gobi. The fluctuation in area, primarily driven by precipitation, is at odds with numerous reports of human-induced desertification in Mongolia and China. There are striking parallels between the vagueness in defining the Gobi and the imprecision and controversy surrounding the Sahara desert’s southern boundary in the 1980s and 1990s. Improved boundary definition has implications for understanding desert “greening” and “browning”, human action and land use, ecological productivity and changing climate parameters in the region. -
Dust Aerosol in Remote Taklimakan Desert and Gobi Deserts of Northwest China Is Thought to Be Hardly Affected by Human Activities, Due to Sparsely Population
General comments: Dust aerosol in remote Taklimakan Desert and Gobi deserts of northwest China is thought to be hardly affected by human activities, due to sparsely population. The authors conducted a comprehensive field measurement in a Gobi farmland region of northwest China, and demonstrated a potential anthropogenic influence on dust physicochemical properties using multiple ground-based active and passive sensors. The agricultural operations and biomass burning from crop residue prior to growing season were well documented to produce significant impacts on elevated dust loadings and absorption characteristics in Dunhuang farmland during spring of 2012. The findings of this study are very interesting and would help to improve our understanding of the interaction among dust aerosol, atmospheric chemistry, and climate change in desert source region. And I suggest that the authors should carry out long-term and continuous measurements of mineral dust at remote Gobi deserts in northwest China, to quantify the potential anthropogenic contributions on regional climatic and environmental changes. I think the English wring is fine, and I recommend this manuscript is appropriate for publishing after minor revision. Minor comments: 1. Abstract, Page 1, line 27: “In the afternoon (13:00–18:00 LT)” ⇒ Change to “In the afternoon (13:00–18:00 LT, local time)”. When an abbreviation firstly appears in the manuscript, please give the full name. 2. Page 3, line 78: “(i.e., hematite and goethite)” ⇒ Change to “(i.e. hematite and goethite)” 3. Page 4, line 90: “(i.e., Mongolia Gobi desert)” ⇒ Change to “(i.e. Inner Mongolian Gobi desert)” 4. Page 4, line 111: “close to the east edge of Kumtag Desert” ⇒ Change to “close to the eastern edge of Kumtag Desert” 5.