CLIMATE in HOT DESERTS Hello Friends
Total Page:16
File Type:pdf, Size:1020Kb

Load more
Recommended publications
-
By H.D.V. PRENDERGAST a Thesis Submitted for the Degree of Doctor of Philosophy of the Australian National University. January 1
STRUCTURAL, BIOCHEMICAL AND GEOGRAPHICAL RELATIONSHIPS IN AUSTRALIAN c4 GRASSES (POACEAE) • by H.D.V. PRENDERGAST A thesis submitted for the degree of Doctor of Philosophy of the Australian National University. January 1987. Canberra, Australia. i STATEMENT This thesis describes my own work which included collaboration with Dr N .. E. Stone (Taxonomy Unit, R .. S .. B.S .. ), whose expertise in enzyme assays enabled me to obtain comparative information on enzyme activities reported in Chapters 3, 5 and 7; and with Mr M.. Lazarides (Australian National Herbarium, c .. s .. r .. R .. O .. ), whose as yet unpublished taxonomic views on Eragrostis form the basis of some of the discussion in Chapter 3. ii This thesis describes the results of research work carried out in the Taxonomy Unit, Research School of Biological Sciences, The Australian National University during the tenure of an A.N.U. Postgraduate Scholarship. iii ACKNOWLEDGEMENTS My time in the Taxonomy Unit has been a happy one: I could not have asked for better supervision for my project or for a more congenial atmosphere in which to work. To Dr. Paul Hattersley, for his help, advice, encouragement and friendship, I owe a lot more than can be said in just a few words: but, Paul, thanks very much! To Mr. Les Watson I owe as much for his own support and guidance, and for many discussions on things often psittacaceous as well as graminaceous! Dr. Nancy Stone was a kind teacher in many days of enzyme assays and Chris Frylink a great help and friend both in and out of the lab •• Further thanks go to Mike Lazarides (Australian National Herbarium, c.s.I.R.O.) for identifying many grass specimens and for unpublished data on infrageneric groups in Eragrostis; Dr. -
The Environmental History and Present Condition of Saudi Arabia's
UNITED STATES DEPARTMENT OF THE INTERIOR GEOLOGICAL SURVEY The environmental history and present condition of Saudi Arabia's northern sand seas by J. W. Whitney I/, D. J. Faulkender, and Meyer Rubin 2/ Open-File Report 83- 7V Prepared for Ministry of Petroleum and Mineral Resources, Deputy Ministry for Mineral Resources Jiddah, Kingdom of Saudi Arabia This report is preliminary and has not been reviewed for conformity with U.S. Geological Survey editorial standards and stratigraphic nomenclature I/ U.S. Geological Survey, Denver, CO 80225 2/ U.S. Geological Survey, Radiocarbon Lab., Reston, VA 22092 1983 CONTENTS Page ABSTRACT................................................ 1 INTRODUCTION............................................ 2 PHYSICAL SETTING AND SEDIMENT SOURCES OF THE SAND SEAS.. 4 AGE AND ORIGIN OF THE SAND SEAS......................... 8 QUATERNARY EOLIAN AND LACUSTRINE DEPOSITS............... 12 Dune systems........................................ 12 Active versus stable dunes.......................... 15 Pleistocene and Holocene lake deposits.............. 18 Diatomite........................................... 24 PRESENT CONDITION OF THE SAND SEAS...................... 25 Precipitation and temperature....................... 25 Vegetation.......................................... 27 Modern and paleo-wind systems....................... 29 ENVIRONMENTAL HISTORY OF THE SAND SEAS.................. 32 DATA STORAGE............................................ 35 REFERENCES CITED........................................ 36 ILLUSTRATIONS -
Great Victoria Desert Dependent Species By: Species Dependent Its and Bioregion Desert Great Victoria the You Conserve Help Can Park
Great Victoria Desert Bioregion resources Photo G.Richardson The Great Victoria Desert bioregion is located in the western half of South Australia and stretches into Western Australia. The desert, after which the bioregion is named, is the largest in Australia. It has an arid climate with warm to extremely hot summers and mild to warm winters. The bioregion receives about 100mm to 250mm of rain per year but, like much of the arid zone, it varies significantly from year to year. Water is a particularly precious resource and only the hardiest of plants and animals can survive in these harsh conditions. In the 1950’s and 60’s, nuclear weapon trials were conducted in the bioregion and several areas were, and remain, contaminated. Biodiversity and habitat The bioregion has dunes and swales with playa lakes, lunettes and rocky areas. There are many types of vegetation including chenopod and samphire shrublands, acacia shrublands and open woodlands, eucalypt open woodlands, casuarina and mallee shrublands and woodlands. Rare or threatened animals include the Malleefowl, Sandhill Dunnart and the Southern Marsupial Mole. 2 | Great Victoria Desert Threats Threats to the Great Victoria Desert bioregion and its dependent For further information species include: Public enquiries • clearance and fragmentation of vegetation by developments such as mining and exploration For more local information on any of the species in this resource please contact your nearest Natural Resource Centre office on: • Overgrazing by feral animals, especially camels and rabbits, and damage to waterholes by camels. Eastwood: (08) 8273 9100 Gawler: (08) 8523 7700 Lobethal: (08) 8389 5900 The Great Victoria Desert bioregion Willunga: (08) 8550 3400 supports most of the known Education enquiries population of Sandhill Dunnarts. -
MVG 16 Acacia Shrublands DRAFT
MVG 16 - ACACIA SHRUBLANDS Acacia hillii, Tanami Desert, NT (Photo: D. Keith) Overview The overstorey of MVG 16 is dominated by multi-stemmed acacia shrubs. The most widespread species is Acacia aneura (mulga). Mulga vegetation takes on a variety of structural expressions and is consequently classified partly within MVG 16 where the overstorey is dominated by multi-stemmed shrubs, partly within MVG 6 in accordance with the Kyoto Protocol definition of forest cover in Australia (trees > 2 m tall and crown cover > 20%, foliage projective cover > 10%); and partly within MVG 13 where the woody dominants are predominantly single-stemmed, but with crown cover less than 20%. Occurs where annual rainfall is below 250mm in southern Australia and below 350mm in northern Australia (Hodgkinson 2002; Foulkes et al. 2014). Species composition varies along rainfall gradients, with substrate and rainfall seasonality (Beadle 1981; Johnson and Burrows 1994). Transitions into MVG 13 Acacia woodlands with higher rainfall and varying soil types. Is most commonly found on red earth soils (Hodgkinson 2002). Facts and figures Major Vegetation Group MVG 16 - Acacia Shrublands Major Vegetation Subgroups 20. Stony mulga woodlands and shrublands NSW, (number of NVIS descriptions) NT, QLD, SA, WA 23. Sandplain Acacia woodlands and shrublands NSW, NT, QLD, SA, WA Typical NVIS structural formations Shrubland (tall, mid,) Open shrubland (tall, mid,) Sparse shrubland (tall, mid,) Number of IBRA regions 53 Most extensive in IBRA region Est. pre-1750 and present : Great Victoria Desert (WA and SA) Estimated pre-1750 extent (km2) 865 845 Present extent (km2) 851 274 Area protected (km2) 85 444 Acacia ligulata (sandhill wattle), SA (Photo: M. -
Flora.Sa.Gov.Au/Jabg
JOURNAL of the ADELAIDE BOTANIC GARDENS AN OPEN ACCESS JOURNAL FOR AUSTRALIAN SYSTEMATIC BOTANY flora.sa.gov.au/jabg Published by the STATE HERBARIUM OF SOUTH AUSTRALIA on behalf of the BOARD OF THE BOTANIC GARDENS AND STATE HERBARIUM © Board of the Botanic Gardens and State Herbarium, Adelaide, South Australia © Department of Environment, Water and Natural Resources, Government of South Australia All rights reserved State Herbarium of South Australia PO Box 2732 Kent Town SA 5071 Australia J. Adelaide Bot. Gard. 18(1): 9-24 (1998) SOIL CRUST LICHENS AND MOSSES ON CALCRETE- DOMINANT SOILS AT MARALINGA IN ARID SOUTH AUSTRALIA D.J. Eldridge Department of Land and Water Conservation, c/- School of Geography, University of New South Wales, Sydney, New South Wales 2052 Abstract A total of 23 lichen and six moss taxa were collected from soil crusts at 15 sites on calcrete-dominant landscapes in the Maralinga area. Apart from two vagant lichens Chondropsis semiviridis (F. Muell. ex Nyl.)Nyl. and Xanthoparmelia convoluta (Krempehl.)Hale, soil lichens were dominated by crustose and squamulose types. Three families, Verrucariaceae, Peltulaceae and Lecideaceae accounted for 57% of the genera found at Maralinga. No liverworts, and only six moss species were collected. Sites with varying disturbance history were used to examine the recovery of crust cover and floristics over time. Across all quadrats, crust cover (± standard error of the mean) averaged 38.0 ± 3.6%. Total crust cover and lichen species richness increased significantly as time since disturbance increased (P<0.001). Field results suggest that recovery of crust cover to levels necessary for protection against water erosion (30-40% cover) is achievable within 30-40 years. -
Desert-2.Pdf
Desert Contens Top Ten Facts PG 1 front cover 1 All Deserts are all different but they all have low amounts of rain PG 2 contens 2 Deserts normally have less than 40 CM a year 3 The Sahara desert is in Northern Africa and is over 12 different countries PG 3 top ten facts 4 Sahara desert is the largest desert in the Earth PG 4 whether and climate 5 Only around 20% of the Deserts on Earth are covered in sand 6 Around one third of the Earth's surface is covered in Desert PG 5 desert map 7 The largest cold Desert on Earth is Antarctica PG 6 animals and people that live there 8 Located in South America, the Atacama Desert is the driest place in the world PG 7 what grows there 9 Lots of animals live in Deserts such as the wild dog 10 The Arabian Desert in the Middle East is the second largest hot desert on Earth but is substantially smaller than the Sahara. This is a list of the deserts in Wether And Climate the world Arabian Desert. ... Kalahari Desert. ... Wether Mojave Desert. ... Sonoran Desert. ... Chihuahuan Desert. ... This is a map showing Deserts are usually very, very dry. Even the wettest deserts get less than ten Thar Desert. ... the deserts in the world inches of precipitation a year. In most places, rain falls steadily throughout the Gibson Desert. year. But in the desert, there may be only a few periods of rains per year with a lot of time between rains. -
The Geography of the Arabian Peninsula
THE GEOGRAPHY OF THE ARABIAN PENINSULA LESSON PLAN: THE GEOGRAPHY OF THE ARABIAN PENINSULA By Joan Brodsky Schur Introduction This lesson introduces students to the physical geography of the Arabian Peninsula, its position relative to bodies of land and water and therefore its role in connecting continents, its climate, and its resources (in the premodern era). Based on evidence from materials provided in four maps and a background essay, students make hypotheses about how human societies adapted to life in a desert climate. Afterwards, they compare their hypotheses to factual evidence. In one concluding activity students are paired as travelers and travel agents. The travelers have specific scholarly interests in visiting the Arabian Peninsula, while the travel agents must plan trips to the peninsula to meet their client’s purposes. In an alternative concluding activity, students study the Arabian camel and the impact of its domestication on human societies in the region. This lesson provides material relevant to understanding the exhibit The Roads of Arabia as well as a second related lesson plan, The Incense Routes: Frankincense and Myrrh, As Good as Gold. Grade Level 5th through 12th grades Time Required Depending upon the number of activities you plan to implement, this lesson takes from one to five class periods. Materials A variety of maps provided in this lesson and others in print and/or online. The background essay provided in this lesson. Essential Questions • What geographical features create the desert climate of the Arabian Desert? • How do land forms and waterways connect different world regions? • How do plants and animals adapt to a desert climate? • How do human societies adapt to living in desert climates? Skills Taught • Reading a variety of types of maps to ascertain specific information. -
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. -
Great Victoria Desert 1
Great Victoria Desert 1 Great Victoria Desert 1 (GVD1 – Great Victoria Desert Shield subregion) BRAD BARTON AND MARK COWAN SEPTEMBER 2001 Subregional description and biodiversity Spinifex (Triodia spp) and mallee (Eucalyptus kingsmillii, values E. youngiana) over hummock grassland dominated by Triodia basedowii occur on the aeolian sand plain. Scattered marble gum (E. gongylocarpa) and native pine Description and area (Callitris) occur on the deeper sands of the sand plains. Mulga and acacia woodlands occur mainly on the The western end of GVD1 is underlain by Yilgarn colluvial and residual soils. Halophytes such as salt bush Craton. There is a higher proportion of sandplains in (Atriplex), Bluebush (Kochia), and samphire comparison to the entire bioregion. To the east is an arid (Arthrocnemum) occur, margins of salt lakes and in saline active sand-ridge desert of deep Quaternary aeolian sands drainage areas. The climate is arid, with summer and overlying Permian and Mesozoic strata of the Officer winter rain approximately 190mm per annum. Basin. Landforms consist of salt lakes and major valley Subregional area is 5, 442, 741ha. floors with lake derived dunes. Sand plains with patches of seif dunes running east west. Areas of moderate relief with out-cropping and silcrete-capped mesas and plateaus Dominant land use (see Appendix B, key b) (breakaways). The subregion contains major a paleo- channel of Ponton Creek. Category Description Percentage of Subregion x Aboriginal Reserve 12.33% xiii Conservation Reserves 7.05% ix Grazing Native Pastures 24.85% xv Other – Lakes and major watercourse 0.09% ix Unallocated Crown Land and Crown Reserves 55.68% Continental Stress Class ocellata), Sandhill Dunnart (Sminthopsis psammophila), Southern Marsupial Mole (Notoryctes typhlops), Mulgara The Continental Stress Class for GVD1 is 6. -
Table 2. Geographic Areas, and Biography
Table 2. Geographic Areas, and Biography The following numbers are never used alone, but may be used as required (either directly when so noted or through the interposition of notation 09 from Table 1) with any number from the schedules, e.g., public libraries (027.4) in Japan (—52 in this table): 027.452; railroad transportation (385) in Brazil (—81 in this table): 385.0981. They may also be used when so noted with numbers from other tables, e.g., notation 025 from Table 1. When adding to a number from the schedules, always insert a decimal point between the third and fourth digits of the complete number SUMMARY —001–009 Standard subdivisions —1 Areas, regions, places in general; oceans and seas —2 Biography —3 Ancient world —4 Europe —5 Asia —6 Africa —7 North America —8 South America —9 Australasia, Pacific Ocean islands, Atlantic Ocean islands, Arctic islands, Antarctica, extraterrestrial worlds —001–008 Standard subdivisions —009 History If “history” or “historical” appears in the heading for the number to which notation 009 could be added, this notation is redundant and should not be used —[009 01–009 05] Historical periods Do not use; class in base number —[009 1–009 9] Geographic treatment and biography Do not use; class in —1–9 —1 Areas, regions, places in general; oceans and seas Not limited by continent, country, locality Class biography regardless of area, region, place in —2; class specific continents, countries, localities in —3–9 > —11–17 Zonal, physiographic, socioeconomic regions Unless other instructions are given, class -
Waste Land (Mewat) in Judea and Samaria Ya'akov Meron
Boston College International and Comparative Law Review Volume 4 | Issue 1 Article 2 5-1-1981 Waste Land (Mewat) in Judea and Samaria Ya'akov Meron Follow this and additional works at: http://lawdigitalcommons.bc.edu/iclr Part of the International Law Commons, and the Land Use Law Commons Recommended Citation Ya'akov Meron, Waste Land (Mewat) in Judea and Samaria, 4 B.C. Int'l & Comp. L. Rev. 1 (1981), http://lawdigitalcommons.bc.edu/iclr/vol4/iss1/2 This Article is brought to you for free and open access by the Law Journals at Digital Commons @ Boston College Law School. It has been accepted for inclusion in Boston College International and Comparative Law Review by an authorized editor of Digital Commons @ Boston College Law School. For more information, please contact [email protected]. Waste Land (Mewat) in Judea and Samaria by Ya 'akov Meron· I. INTRODUCTION The Agreement between Egypt and Israel calling for autonomy to the Pales tinians, I as well as Israel's continued policy of establishing settlements, have brought to the forefront of international concerns questions pertaining ap parently to private law. Not long before the official opening of the negotiations concerning the future of the Palestinian Arabs, a high ranking American diplomat stated that one of the basic iss~es to be resolved was: "who controls the [public] lands ... , who has the authority to transfer the land, [and] who has authority to [a]ppropriate the land."2 Bold statements have been made with regard to the legality of the settlements established by Israel. It is the author's submission that talk about "expropriation" is largely beside the point.