Sonoran Desert Management Questions
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Cultural Landscape Planning: the Mexicali Valley, Mexico
The Sustainable City VII, Vol. 1 457 Cultural landscape planning: the Mexicali Valley, Mexico R. I. Rojas-Caldelas1, C. A. Pena-Salmon1 & J. Ley-Garcia2 1Faculty of Architecture and Design, Autonomous University of Baja California, Mexicali, México 2Institute of Research in Social Sciences, Autonomous University of Baja California, Mexicali, México Abstract Initiating around the eighties, the academic training of landscape architects in Mexico is quite recent compared with the tradition in Europe and the U.S. Also new, is the development of landscape research conducted mainly by geographers, urban planners and other professionals trained in natural sciences, whose work is primarily oriented to land use management for urban development and conservation of natural resources or cultural heritage purposes. However, the issue of the cultural landscape in Mexico has been little explored and lacks any integrated and multidisciplinary methodology to bring together social, cultural and natural processes for study. Therefore, this work focuses on the presentation of an appropriate methodology to address the issue of the evolving cultural landscape of the Valley of Mexicali. This work has been developed into three stages: characterization, multiple assessment of landscape and integration of strategies for their management. Thus progress will be presented for the characterization of physical units, landscape components through pictures, visual and spatial patterns of landscape that structure the region and its settlements. As a partial result it was found that multi-valued zones visually and spatially exist in the Mexicali Valley, as well as activities that give character and differentiate it from other agricultural areas of Baja California. Keywords: cultural landscape, landscape assessment methodologies, visual and spatial assessment, sustainable landscape planning. -
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 -
Ecoregions of Nevada Ecoregion 5 Is a Mountainous, Deeply Dissected, and Westerly Tilting Fault Block
5 . S i e r r a N e v a d a Ecoregions of Nevada Ecoregion 5 is a mountainous, deeply dissected, and westerly tilting fault block. It is largely composed of granitic rocks that are lithologically distinct from the sedimentary rocks of the Klamath Mountains (78) and the volcanic rocks of the Cascades (4). A Ecoregions denote areas of general similarity in ecosystems and in the type, quality, Vegas, Reno, and Carson City areas. Most of the state is internally drained and lies Literature Cited: high fault scarp divides the Sierra Nevada (5) from the Northern Basin and Range (80) and Central Basin and Range (13) to the 2 2 . A r i z o n a / N e w M e x i c o P l a t e a u east. Near this eastern fault scarp, the Sierra Nevada (5) reaches its highest elevations. Here, moraines, cirques, and small lakes and quantity of environmental resources. They are designed to serve as a spatial within the Great Basin; rivers in the southeast are part of the Colorado River system Bailey, R.G., Avers, P.E., King, T., and McNab, W.H., eds., 1994, Ecoregions and subregions of the Ecoregion 22 is a high dissected plateau underlain by horizontal beds of limestone, sandstone, and shale, cut by canyons, and United States (map): Washington, D.C., USFS, scale 1:7,500,000. are especially common and are products of Pleistocene alpine glaciation. Large areas are above timberline, including Mt. Whitney framework for the research, assessment, management, and monitoring of ecosystems and those in the northeast drain to the Snake River. -
Synoptic-Scale Control Over Modern Rainfall and Flood Patterns in the Levant Drylands with Implications for Past Climates
JUNE 2018 ARMONETAL. 1077 Synoptic-Scale Control over Modern Rainfall and Flood Patterns in the Levant Drylands with Implications for Past Climates MOSHE ARMON Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University of Jerusalem, Givat Ram, Jerusalem, Israel ELAD DENTE Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University of Jerusalem, Givat Ram, and Geological Survey of Israel, Jerusalem, Israel JAMES A. SMITH Department of Civil and Environmental Engineering, Princeton University, Princeton, New Jersey YEHOUDA ENZEL AND EFRAT MORIN Fredy and Nadine Herrmann Institute of Earth Sciences, Hebrew University of Jerusalem, Givat Ram, Jerusalem, Israel (Manuscript received 23 January 2018, in final form 1 May 2018) ABSTRACT Rainfall in the Levant drylands is scarce but can potentially generate high-magnitude flash floods. Rainstorms are caused by distinct synoptic-scale circulation patterns: Mediterranean cyclone (MC), active Red Sea trough (ARST), and subtropical jet stream (STJ) disturbances, also termed tropical plumes (TPs). The unique spatiotemporal char- acteristics of rainstorms and floods for each circulation pattern were identified. Meteorological reanalyses, quantitative precipitation estimates from weather radars, hydrological data, and indicators of geomorphic changes from remote sensing imagery were used to characterize the chain of hydrometeorological processes leading to distinct flood patterns in the region. Significant differences in the hydrometeorology of these three flood-producing synoptic systems were identified: MC storms draw moisture from the Mediterranean and generate moderate rainfall in the northern part of the region. ARST and TP storms transfer large amounts of moisture from the south, which is converted to rainfall in the hyperarid southernmost parts of the Levant. -
Imperial Irrigation Decision Support System Summary Report
Draft Imperial Irrigation Decision Support System Summary Report Prepared for Imperial Irrigation District December 2001 2525 Airpark Drive Redding, California In Association with: Keller-Bliesner Engineering Davids Engineering Colorado State University Allen Engineering Contents Section Page 1.0 Introduction.........................................................................................................................1-1 IID Irrigation and Drainage Systems................................................................................1-1 Water Transfer Basics..........................................................................................................1-4 Imperial Irrigation Decision Support System..................................................................1-5 IID System Representation....................................................................................1-5 IIDSS Purpose .........................................................................................................1-5 Peer Review..........................................................................................................................1-6 2.0 Design of the Imperial Irrigation Decision Support System.....................................2-1 Irrigation System Overview...............................................................................................2-1 Delivery System......................................................................................................2-3 On-farm System......................................................................................................2-3 -
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. -
Rose-Marcella-Thesis-2020.Pdf
CALIFORNIA STATE UNIVERSITY, NORTHRIDGE Nebkha Morphology, Distribution and Stability Black Rock Playa, Nevada A thesis submitted in partial fulfillment of the requirements For the degree of Master of Arts in Geography By Marcella Rose December 2019 The thesis of Marcella Rose is approved: _______________________________________ _____________ Dr. Julie Laity Date _______________________________________ _____________ Dr. Thomas Farr Date _______________________________________ _____________ Dr. Amalie Orme, Chair Date California State University, Northridge ii Acknowledgements Dr. Orme, I really don’t think that there is a sufficient combination of words that exist to properly express the immense amount of gratitude I feel for everything that you have done for me. This college education changed my life for the better and I hope you realize what a significant role you were within that experience. I am thankful that not only did I get a great professor, but also a friend. Dr. Laity, thank you so much for having faith in me and for taking me on as one of your last students to advise. But most of all, thank you for pushing me to be better – I needed that. Dr. Farr, I was so excited during DEVELOP that you accepted to be a part of my committee. It was a pleasure to work with you within the Black Rock Playa research team but then to also take our research a step further for this graduate thesis. I would also like to thank the staff at the Bureau of Land Management, Winnemucca: Dr. Mark E. Hall, Field Manager of the Black Rock Field Office; Shane Garside, Black Rock Station Manager/ Outdoor Recreation Planner; Brian McMillan, Rangeland Management Technician; and Braydon Gaard, Interim Outdoor Recreation Planner. -
Mojave Desert Native Plant Program Mojave Desert Restoration Challenges: It’S Hot and Dry!
Mojave Desert Native Plant Restoration Following Wildfires and Weed Treatments: T HE RIGHT S EED IN THE RIGHT PLACE JJ Smith Mojave Desert Ecoregion Loss of Mojave Desert Tortoise Habitat Federally Threatened (listed 1990) Species decline through most of range Red brome, cheatgrass, Mediterranean grasses – poor nutritional value Large, severe fires – habitat loss, spread of annual invasive grasses Habitat restoration identified as highest priority by USFWS Recovery Implementation Teams (RITs). Invasive Annual Grasses and Fuel Continuity Aleta Nafus – BLM Southern Nevada District Lynn Sweet – University of California Riverside • Over 1 million acres burned since 2005 (Mojave Desert Initiative 2010) • 2,307,068 acres burned at least once since 1980 (Mojave Basin and Range REA, NatureServe 2013) Loss of Native Species from Soil Seed Banks Todd C. Esque, James A. Young, C. Richard Tracy. 2010. Short-term effects of experimental fires on a Mojave Desert seed bank. Journal of Arid Environments, 74: 1302-1308. • Fire depleted both native and non-native seed densities • Native seed densities were significantly lower than non-native seed densities both before and after fire National Seed Strategy for Rehabilitation and Restoration ➢ Congress created Native Plant Materials Development Programs in response to catastrophic wildfires in 1998 and 1999 ➢ Builds on 15+ years of work ➢ National Seed Strategy announced August 2015 ➢ Calls for an Unprecedented Level of Collaboration ➢ Developed by the Plant Conservation Alliance (PCA) ➢ Only country in the world with a National Seed Strategy 6 Plant Conservation Alliance Federal Committee 12 Federal Agencies Federal Committee – led by BLM PCA also includes ➢ 325 Non-federal Partners ➢ 9 International Partners 7 National Seed Strategy “The right seed in the right place at the right time.” Goal 1 : Identify seed needs and ensure the reliable availability of genetically appropriate seed. -
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. -
Salinity of Surface Water in the Lower Colorado River Salton Sea Area
Salinity of Surface Water in The Lower Colorado River Salton Sea Area GEOLOGICAL SURVEY PROFESSIONAL PAPER 486-E Salinity of Surface Water in The Lower Colorado River- Salton Sea Area By BURDGE IRELAN WATER RESOURCES OF LOWER COLORADO RIVER SALTON SEA AREA GEOLOGICAL SURVEY PROFESSIONAL PAPER 486-E UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON : 1971 UNITED STATES DEPARTMENT OF THE INTERIOR ROGERS C. B. MORTON, Secretary GEOLOGICAL SURVEY William T. Pecora, Director Library of Congress catalog-card No. 72 610761 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 Price 50 cents (paper cover) CONTENTS Page Page Abstract . _.._.-_. ._...._ ..._ _-...._ ...._. ._.._... El Ionic budget of the Colorado River from Lees Ferry to Introduction .._____. ..... .._..__-. - ._...-._..__..._ _.-_ ._... 2 Imperial Dam, 1961-65 Continued General chemical characteristics of Colorado River Tapeats Creek .._________________.____.___-._____. _ E26 water from Lees Ferry to Imperial Dam ____________ 2 Havasu Creek __._____________-...- _ __ -26 Lees Ferry .._._..__.___.______.__________ 4 Virgin River ..__ .-.._..-_ --....-. ._. 26 Grand Canyon ................._____________________..............._... 6 Unmeasured inflow between Grand Canyon and Hoover Dam ..........._._..- -_-._-._................-._._._._... 8 Hoover Dam .__-.....-_ .... .-_ . _. 26 Lake Havasu - -_......_....-..-........ .........._............._.... 11 Chemical changes in Lake Mead ............-... .-.....-..... 26 Imperial Dam .--. ........_. ...___.-_.___ _.__.__.._-_._.___ _ 12 Bill Williams River ......._.._......__.._....._ _......_._- 27 Mineral burden of the lower Colorado River, 1926-65 . -
New and Alamo River Wetlands Master Plan Revised Final Report May 21, 2007
NEW AND ALAMO RIVER WETLANDS MASTER PLAN REVISED FINAL REPORT MAY 21, 2007 Prepared for: Wildlife Conservation Board Salton Sea Authority Sacramento, CA La Quinta, CA Prepared by: Tetra Tech, Inc. Wetlands Management Services Lafayette, CA Chelsea, MI New and Alamo River Wetlands Master Plan Revised Final Report May 21, 2007 Prepared for: Wildlife Conservation Board Salton Sea Authority 1807 13th Street, Suite 103 78-401 Highway 111, Suite T Sacramento, CA 95814 La Quinta, CA 92253 Prepared by: Tetra Tech, Inc. Wetlands Management Services 3746 Mt. Diablo Blvd., Suite 300 6995 Westbourne Dr. Lafayette, CA 94549 Chelsea, MI 48118 New and Alamo River Wetland Master Plan, Final Report Table of Contents Executive Summary .................................................................................................... ES-1 1. Introduction.......................................................................................................1-1 1.1 Summary of Prior Work............................................................................................................1-1 1.2 Organization of Master Plan Report .......................................................................................1-6 2. Historical Water Quality Data in the Alamo and New River Basins..........2-1 2.1 New and Alamo River Flow......................................................................................................2-1 2.2 Water Quality – New River......................................................................................................2-5 -
Selenium Roy A
Nutrient Dynamics in the Salton Basin- Implications from Calcium, Uranium, Molybdenum, and Selenium Roy A. Schroeder, U. S. Geological Survey, San Diego, California and Willian H. Orem, U.S. Geological Survey, Reston, Virginia H31B-02 ABSTRACT: The Salton Sea has been accumulating chemical constituents delivered by its tributary streams for nearly 100 years because it has no outlet. The buildup of chemicals that are highly soluble and unreactive, such as chloride, has resulted in the development of a quasi- marine lake. In contrast, chemicals that react to form insoluble phases ultimately enter the sediment that accumulates on the floor of the Sea. Solubility properties are especially relevant for two important contaminants, selenium and nitrogen. The selenium is contained in Colorado River water used for irrigation, and nitrogen is derived mostly from chemical fertilizer in agricultural runoff. Both are delivered to the Salton Sea as highly soluble oxyanions by the Alamo and New Rivers, which are relatively high in dissolved oxygen at their outlets to the Salton Sea, but are removed as reduced species in anoxic sediment on the Sea’s floor. Without this removal mechanism, selenium concentration would presently be about 400 micrograms per liter and nitrogen would be about 100 milligrams per liter in the Salton Sea’s water, rather than the observed concentrations of only about 1 microgram per liter and 5 milligrams per liter, respectively. Ironically, anoxic conditions responsible for producing the noxious odors and low oxygen conditions that lead to periodic dieoffs of large numbers of fish in the Salton Sea have prevented aqueous selenium and nitrogen from reaching levels that could indeed pose an extreme environmental hazard.