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One of Five West Coast, Low-Latitude Deserts of the World, the Namib Extends Along the Entire Namibian Coastline in an 80-120 Km Wide Belt
N A M I B I A G 3 E 0 O 9 1 L - O Y G E I V C R A U S L NAMIB DESERT Source: Roadside Geology of Namibia One of five west coast, low-latitude deserts of the world, the Namib extends along the entire Namibian coastline in an 80-120 km wide belt. Its extreme aridity is the result of the cold, upwelling Benguela Current, which flows up the west coast of Africa as far as Angola, and because of its low temperatures induces very little evaporation and rainfall (<50 mm per year). It does, however, create an up to 50 km wide coastal fog belt providing sufficient moisture for the development of a specialist flora and fauna, many of which are endemic to the Namib. In addition, the lagoons at Walvis Bay and Sandwich Harbour are designated wetlands of international importance, because of their unique setting and rich birdlife, including flamingo, white pelican and Damara tern. Larger mammals like the famed desert elephant, black rhino, lion, cheetah and giraffe can be found along the northern rivers traversing the Skeleton Coast National Park. Geomorphologically, the Namib includes a variety of landscapes, including classic sand dunes, extensive gravel plains, locally with gypcrete and calcrete duricrusts, elongated salt pans, ephemeral watercourses forming linear oases, inselbergs and low mountain ranges. Along the coast, wind-swept sandy beaches alternate with rocky stretches, in places carved into striking rock formations (e.g. Bogenfels Arch). Designated a UNESCO World Heritage Site in 2013, the “Namib Sand Sea“ between Lüderitz and the Kuiseb River encompasses such well-known landmarks as Sossusvlei and Sandwich Harbour, while the fabled Skeleton Coast north of the Ugab River is notorious for its numerous ship wrecks. -
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 -
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 ........................................................ -
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. -
The Effect of Weather Conditions on the Seasonal Variation of Physical Activity
PHYSICAL ACTIVITY IN THE ARAB REGION THE EFFECT OF WEATHER CONDITIONS ON THE SEASONAL VARIATION OF PHYSICAL ACTIVITY – Written by Abdulla Saeed Al-Mohannadi and Mohamed Ghaith Al-Kuwari, Qatar Physical inactivity is considered the role on physical activity in regions with a walking, cycling and outdoor sports have fourth top risk factor for death worldwide. temperate climate – even on day-to-day been identified as the main source for Approximately 3.2 million of world’s basis4. accumulating the recommended amount population die each year due to insufficient Several studies have investigated of daily physical activity. Studies have physical activity1. Regular physical activity obstacles to participation in physical found that time spent outdoors is highly can decrease the risk of developing activity. These studies have identified non-communicable diseases such as adverse weather conditions such as extreme hypertension, type 2 diabetes, some types temperatures, hours of daylight, snow, rain time spent of cancers and depression2. Prevalence of and wind as major barriers for participation insufficient physical activity was highest in in physical activity. Further, adverse weather outdoors is highly the World Health Organization regions of the conditions are responsible for the seasonal correlated with Americas and the Eastern Mediterranean variation observed in physical activity for (50% of women, 40% of men)2. all individuals regardless of age5. The aim of certain weather Physical environmental factors have this review is to summarise the relationship been considered contributing determinants between weather conditions and level of conditions, such of health and factors that enable or disable physical activity. as high or low individuals from participating in daily physical activity. -
The K-Index Is One of the Main Stability Indices That We Use to Determine the Probability of Thunderstorm Activity in Our Area
The K-Index is one of the main stability indices that we use to determine the probability of thunderstorm activity in our area. The American Meteorology Society’s (AMS) Glossary of Meteorology defines a stability index as: “Any of several quantities that attempt to evaluate the potential for convective storm activity and that may be readily evaluated from operational sounding data.” AMS (2017) i.e. weather balloon data. High pressure generally is associated with a stable atmosphere and a minimized chance of showers and thunderstorms. Low pressure is generally associated with an unstable atmosphere and an increased chance of showers and thunderstorms. The K-Index is thus defined “K-index: This index is due to George (1960) and is defined by The first term is a lapse rate term, while the second and third are related to the moisture between 850 and 700 mb, and are strongly influenced by the 700-mb temperature–dewpoint spread. As this index increases from a value of 20 or so, the likelihood of showers and thunderstorms is expected to increase.” AMS(2017) In simpler terms, the K-Index evaluates the change in temperature from 850mb in height to 500mb in height, adds the dewpoint at 850mb in height and then subtracts the difference of the temperature and dewpoint at 700mb in height. This relationship between temperature and moisture is one way to measure stability. In Bermuda, a value of 30 or higher suggests at least a moderate risk of airmass thunderstorms. Bermuda Weather Service (BWS) (2017) There are many other stability indices that can be calculated from weather balloon and weather model data. -
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. -
What Is in a Desert?
What is in a Desert? A Kindergarten Field Trip to Red Rock Canyon National Conservation Area Las Vegas, Nevada What is in a Desert? Overview: Students will use a variety of senses and activities to learn about what makes a desert. Animals, plants, rocks, and cultural relationships will be explored using the Visitor Center at Red Rock Canyon National Conservation Area. Students will also use observations to describe patterns of what plants and animals need to survive. Duration: 25-minute session for pre-activity 1 day for field trip and reflection 30-minute session for post-activity Grade: Kindergarten Next Generation Science Standards: Field Trip Theme: Red Rock Canyon National Conservation Area offers a great opportunity to see the diverse collection of plants, animals, and rocks found in the Mojave Desert. During this field trip, students will use their senses and make observations on the plants, animals, and rocks of Red Rock Canyon. Objectives: Students will: ▪ identify at least two desert animals. ▪ identify at least two desert plants. ▪ identify at least two types of rocks. ▪ use their senses to explore the elements that make up a desert. ▪ describe various ways that desert animals find what they need to survive in the desert. ▪ use observations to describe patterns of what plants and animals need to survive. Background Information: Although at first glance the Mojave Desert may seem an unlikely place for animals and plants to thrive or even exist, it actually contains sizeable populations of a diverse number of species. Because desert species have adapted to their environment, these are the habitats in which they thrive. -
The Impact of ENSO in the Atacama Desert and Australian Arid Zone: Exploratory Time-Series Analysis of Archaeological Records
Chungara, Revista de Antropología Chilena ISSN: 0716-1182 [email protected] Universidad de Tarapacá Chile Williams, Alan; Santoro, Calogero M.; Smith, Michael A.; Latorre, Claudio The impact of ENSO in the Atacama desert and Australian arid zone: exploratory time-series analysis of archaeological records Chungara, Revista de Antropología Chilena, vol. 40, 2008, pp. 245-259 Universidad de Tarapacá Arica, Chile Available in: http://www.redalyc.org/articulo.oa?id=32609903 How to cite Complete issue Scientific Information System More information about this article Network of Scientific Journals from Latin America, the Caribbean, Spain and Portugal Journal's homepage in redalyc.org Non-profit academic project, developed under the open access initiative The impact of ENSO in the Atacama Desert and Australian arid zone:Volumen Exploratory 40 Número time-series Especial, analysis… 2008. Páginas 245-259245 Chungara, Revista de Antropología Chilena THE IMPACT OF ENSO IN THE ATACAMA DESERT AND AUSTRALIAN ARID ZONE: EXPLORATORY TIME-SERIES ANALYSIS OF ARCHAEOLOGICAL RECORDS1 EL IMPACTO DE ENSO EN EL DESIERTO DE ATACAMA Y LA ZONA ÁRIDA DE AUSTRALIA: ANÁLISIS EXPLORATORIOS DE SERIES TEMPORALES ARQUEOLÓGICAS Alan Williams2, Calogero M. Santoro3, Michael A. Smith4, and Claudio Latorre5 A comparison of archaeological data in the Atacama Desert and Australian arid zone shows the impact of the El Niño-Southern Oscillation (ENSO) over the last 5,000 years. Using a dataset of > 1400 radiocarbon dates from archaeological sites across the two regions as a proxy for population change, we develop radiocarbon density plots, which are then used to explore the responses of these prehistoric populations to ENSO climatic variability. -
Mower County, MN
Natural Hazards Assessment Mower County, MN Prepared by: NOAA / National Weather Service La Crosse, WI 1 Natural Hazards Assessment for Mower County, MN Prepared by NOAA / National Weather Service – La Crosse Last Update: October 2013 Table of Contents: Overview…………………………………………………. 3 Tornadoes………………………………………………… 4 Severe Thunderstorms / Lightning……….…… 5 Flooding and Hydrologic Concerns……………. 6 Winter Storms and Extreme Cold…….…….…. 7 Heat, Drought, and Wildfires………………….... 8 Local Climatology……………………………………… 9 National Weather Service & Weather Monitoring……………………….. 10 Resources………………………………………………… 11 2 Natural Hazards Assessment Mower County, MN Prepared by National Weather Service – La Crosse Overview Mower County is in the Upper Mississippi River Valley of the Midwest with rolling hills and relatively flat farm land. The City of Austin is an urban area on the far western end of the county. The area experiences a temperate climate with both warm and cold season extremes. Winter months can bring occasional heavy snows, intermittent freezing precipitation or ice, and prolonged periods of cloudiness. While true blizzards are rare, winter storms impact the area on average about 4 times per season. Occasional arctic outbreaks bring extreme cold and dangerous wind chills. Thunderstorms occur on average 30 to 50 times a year, mainly in the spring and summer months. The strongest storms can produce associated severe weather like tornadoes, large hail, or damaging wind. Both river flooding and flash flooding can occur, along with urban-related flood problems. Heat and high humidity is occasionally observed in June, July, or August. The autumn season usually has the quietest weather. Dense fog occurs several times during mainly the fall or winter months. High wind events can also occur from time to time, usually in the spring or fall. -
What Is Antarctica?
What Is Antarctica? What Is Antarctica? This text is from the "NASA Knows!" series from NASA. Antarctica is a continent. It is Earth's fifth-largest continent and is covered almost completely in ice. Antarctica covers Earth's South Pole. What Is Antarctica Like? NASA Antarctica is Earth's fifth largest continent. Antarctica is the coldest place on Earth. The average temperature in Antarctica in the winter is minus 34.4 Celcius (minus 30 degrees Fahrenheit). The temperature in the center of Antarctica is much lower than the temperature on the coasts. The lowest temperature ever recorded in Antarctica was minus 89.4 C (minus 129 F). The highest temperature ever recorded in Antarctica was 15 C (59 F). Antarctica has just two seasons: summer and winter. Antarctica has six months of daylight in its summer and six months of darkness in its winter. The seasons are caused by the tilt of Earth's axis in relation to the sun. The direction of the tilt never changes. But as the Earth orbits the sun, different parts of the planet are exposed to direct sunlight. During summer, Antarctica is on the side of Earth tilted toward the sun and is in constant sunlight. In the winter, Antarctica is on the side of Earth tilted away from the sun, causing the continent to be dark. Antarctica is considered a desert because it receives very little rain or snowfall. The small amount of snow that does fall does not melt but builds up over hundreds and thousands of years to form large, thick ice sheets. -
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.