Energy from the Desert
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Australia: State of the Environment 1996: Chapter 4
Chapter 4 . Biodiversity ‘Still Flying’ from the painting of a Wandering Albatross by Richard Prepared by Weatherly. Denis Saunders (Chair), CSIRO Division of Wildlife and Ecology Andrew Beattie, Centre for Biodiversity and Bioresources, School of Biological Sciences, Macquarie University Susannah Eliott (Research Assistant/Science Writer), Centre for Science Communication, University of Technology, Sydney Marilyn Fox, School of Geography, University of New South Wales Burke Hill, CSIRO Division of Fisheries Bob Pressey, New South Wales National Parks and Wildlife Service Duncan Veal, Centre for Biodiversity and Bioresources, School of Biological Sciences, Macquarie University Jackie Venning, State of Environment Reporting, South Australian Department of Environment and Natural Resources Mathew Maliel (State of the Environment Reporting Unit member), Department of the Environment, Sport and Territories (Facilitator) Charlie Zammit (former State of the Environment Reporting Unit member), Department of the Environment, Sport and Territories (former Facilitator) 4-1 . Australia: State of the Environment 1996 . Contents Introduction. 4-4 Pressure . 4-7 Human populations . 4-9 Urban development . 4-9 Tourism and recreation . 4-9 Harvesting resources and land use. 4-10 Fisheries . 4-10 Forestry . 4-11 Pastoralism. 4-12 Agriculture . 4-12 Introduced species . 4-16 Vertebrates . 4-16 Invertebrates. 4-17 Plants. 4-18 Micro-organisms. 4-20 Native species out of place . 4-20 Pollution . 4-21 Mining . 4-22 Climate change . 4-22 State . 4-23 The state of ecosystem diversity . 4-23 Biogeographic regionalisations for Australia . 4-23 Ecosystem diversity. 4-26 The state of species diversity. 4-30 Number and distribution of species . 4-31 Status of species . -
Evidence of Altered Fire Regimes in the Western Desert Region of Australia
272 Conservation Science W. Aust. 5 (3)N.D. : 272–284 Burrows (2006) et al. Evidence of altered fire regimes in the Western Desert region of Australia N.D. BURROWS1, A.A. BURBIDGE2, P.J. FULLER3 AND G. BEHN1 1Department of Conservation and Land Management, Locked Bag 104, Bentley Delivery Centre, Bentley, Western Australia, 6983. 2Department of Conservation and Land Management, Western Australian Wildlife Research Centre, P.O. Box 51, Wanneroo, Western Australia, 6946. 33 Willow Rd, Warwick, Western Australia, 6024. SUMMARY and senescing vegetation or vast tracts of vegetation burnt by lightning-caused wildfires. The relatively recent exodus of Aboriginal people from parts of the Western Desert region of Australia has coincided with an alarming decline in native mammals INTRODUCTION and a contraction of some fire sensitive plant communities. Proposed causes of these changes, in what The Great Victoria, Gibson, Great Sandy and Little Sandy is an otherwise pristine environment, include an altered Deserts (the Western Desert) occupy some 1.6 million fire regime resulting from the departure of traditional km2 of Western Australia, of which more than 100 000 Aboriginal burning, predation by introduced carnivores km2 is managed for nature conservation. The and competition with feral herbivores. conservation reserves in the Western Desert are large, Under traditional law and custom, Aboriginal people remote and relatively undisturbed. A management option inherit, exercise and bequeath customary responsibilities for such reserves is not to intervene -
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. -
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. -
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. -
The Vegetation of the Western Australian Deserts
©Reinhold-Tüxen-Gesellschaft (http://www.reinhold-tuexen-gesellschaft.de/) Ber. d. Reinh.-Tüxen-Ges. 18, 219-228. Hannover 2006 The Vegetation of the Western Australian Deserts - Erika and Sandro Pignatti, Rom - Abstract The internal area of W. Australia has arid climate and conditions for plant growth are particularly difficult. The surface of this huge, almost uninhabited territory consists of four landscape systems: the Great Sandy Desert, the Little Sandy Desert, the Great Victoria Desert, the Gibson Desert. The four deserts extend between 21-26° of south- ern latitude, linking to the central Australian deserts and the Nullarbor Plain in the South. Meteorological stations are only in settlements of the surrounding semi-desert areas (Wiluna, Meekatharra, Cue, Warburton), and all show around 200-250 mm year- ly rainfall; in the centre of the deserts rainfall is still much lower, and indicated as “erratic and unreliable”; some areas may lack rain for several years. Despite of the par- ticularly severe ecological conditions, most of the surface is covered by vegetation (at least a discontinuous one) and during expeditions in 2001 and 2002 over 700 species were collected and more than 350 phytosociological relevés were carried out.Two main habitat types can be recognized: Mulga – scattered growth of treelets (Acacia aneura, generally about 3-4 m height), with open understorey (Senna, Eremophila, Solanum) and herbs usually covering less than 20 % of the surface; in the Gibson Desert mulga occurs mainly on hard rock sub- strate (granite, laterite). Because of the discontinuous plant cover, fire can spread only over limited areas. Spinifex – Quite a compact cover of perennial grasses (several species of Triodia, with sharply pointed leaves in dense tussocks 3-5 dm high, panicles up to 1 m and high- er) in monospecific populations covering 60-80 % of the surface; in the sandy deserts, on siliceous sand. -
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. -
Lay of the Land I
Laojunshan National Park. Photo by Xu Jian PART 1: LAY OF THE LAND I. Biodiversity This part of the book provides context for land protection efforts in China aimed at protecting biodiversity. Chapter I, Biodiversity, provides an overview of the country’s wealth of species and ecosystem values. Because ample existing literature thoroughly documents China’s biodiversity resources, this chapter does not delve into great detail. Rather, it provides a brief overview of species diversity, and then describes the locations, types, and conservation issues associated with each major ecosystem. Chapter II, Land Use, identifies the locations and trends in land use across the country, such as urbanization, livestock grazing, forest uses, and energy development, which can affect multiple ecosystems. Not surprisingly, China’s flora and fauna are experiencing ever- increasing impacts as a result of China’s unprecedented economic growth and exploding demand for natural resources. Thus, new and strengthened land protection efforts are required to ensure the persistence of China’s rich biodiversity heritage (see Part 3, Land Protection in Practice). A. Species Diversity Terrestrial biodiversity in China is among the highest in the world, and research and inventories of the distribution and status of the country’s biodiversity are fairly comprehensive. China is home to 15% of the world’s vertebrate species including wildlife such as the Yunnan golden monkey, black-necked crane, and the iconic giant panda. China also accounts for 12% of all plant species in the world, ranked third in the world for plant diversity with 30,000 species (Chinese Academy of Sciences, 1992) (Li et al., 2003). -
Inverted Relief Landforms in the Kumtagh Desert of Northwestern China: a Mechanism to Estimate Wind Erosion Rates
GEOLOGICAL JOURNAL Geol. J. 52: 131–140 (2017) Published online 13 November 2015 in Wiley Online Library (wileyonlinelibrary.com). DOI: 10.1002/gj.2739 Inverted relief landforms in the Kumtagh Desert of northwestern China: a mechanism to estimate wind erosion rates ZHEN-TING WANG1,2*, ZHONG-PING LAI3 and JIAN-JUN QU2 1State Key Laboratory of Earth Surface Processes and Resource Ecology, Beijing Normal University, Beijing, China 2Dunhuang Gobi Desert Research Station, Cold and Arid Regions Environmental and Engineering Research Institute, CAS, Dunhuang, China 3State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan, China Although commonly found in deserts, our knowledge about inverted relief landforms is very limited. The so-called ‘Gravel Body’ in the northern Kumtagh Desert is an example of an inverted relief landform created by the exhumation of a former fluvial gravel channel. The common occurrence of these landforms indicates that fluvial processes played an important role in shaping the Kumtagh Desert in the past 151 ka. A physical model is presented to reconstruct the palaeohydrology of these fluvial channels in terms of several measurable parameters including terrain slope, boulder size, and channel width. Combining the calculated palaeoflood depth, the maximal depth of channel bed eroded by wind, and the current height of inverted channels with the age of the aeolian sediments covered by gravels, the local wind erosion rate is estimated to be 0.21–0.28 mm/year. It is shown that wind erosion occurring in the Kumtagh Desert is no more severe than in adjacent regions. Since the modern Martian environment is very similar to that of hyperarid deserts on Earth, and Mars was once subjected to fluvial processes, this study will be helpful for understanding the origin of analogous Martian surface landforms and their causative processes.