Physical Limits of Flight Performance in the Heaviest Soaring Bird
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Understanding the Value of Arts & Culture | the AHRC Cultural Value
Understanding the value of arts & culture The AHRC Cultural Value Project Geoffrey Crossick & Patrycja Kaszynska 2 Understanding the value of arts & culture The AHRC Cultural Value Project Geoffrey Crossick & Patrycja Kaszynska THE AHRC CULTURAL VALUE PROJECT CONTENTS Foreword 3 4. The engaged citizen: civic agency 58 & civic engagement Executive summary 6 Preconditions for political engagement 59 Civic space and civic engagement: three case studies 61 Part 1 Introduction Creative challenge: cultural industries, digging 63 and climate change 1. Rethinking the terms of the cultural 12 Culture, conflict and post-conflict: 66 value debate a double-edged sword? The Cultural Value Project 12 Culture and art: a brief intellectual history 14 5. Communities, Regeneration and Space 71 Cultural policy and the many lives of cultural value 16 Place, identity and public art 71 Beyond dichotomies: the view from 19 Urban regeneration 74 Cultural Value Project awards Creative places, creative quarters 77 Prioritising experience and methodological diversity 21 Community arts 81 Coda: arts, culture and rural communities 83 2. Cross-cutting themes 25 Modes of cultural engagement 25 6. Economy: impact, innovation and ecology 86 Arts and culture in an unequal society 29 The economic benefits of what? 87 Digital transformations 34 Ways of counting 89 Wellbeing and capabilities 37 Agglomeration and attractiveness 91 The innovation economy 92 Part 2 Components of Cultural Value Ecologies of culture 95 3. The reflective individual 42 7. Health, ageing and wellbeing 100 Cultural engagement and the self 43 Therapeutic, clinical and environmental 101 Case study: arts, culture and the criminal 47 interventions justice system Community-based arts and health 104 Cultural engagement and the other 49 Longer-term health benefits and subjective 106 Case study: professional and informal carers 51 wellbeing Culture and international influence 54 Ageing and dementia 108 Two cultures? 110 8. -
Soaring Weather
Chapter 16 SOARING WEATHER While horse racing may be the "Sport of Kings," of the craft depends on the weather and the skill soaring may be considered the "King of Sports." of the pilot. Forward thrust comes from gliding Soaring bears the relationship to flying that sailing downward relative to the air the same as thrust bears to power boating. Soaring has made notable is developed in a power-off glide by a conven contributions to meteorology. For example, soar tional aircraft. Therefore, to gain or maintain ing pilots have probed thunderstorms and moun altitude, the soaring pilot must rely on upward tain waves with findings that have made flying motion of the air. safer for all pilots. However, soaring is primarily To a sailplane pilot, "lift" means the rate of recreational. climb he can achieve in an up-current, while "sink" A sailplane must have auxiliary power to be denotes his rate of descent in a downdraft or in come airborne such as a winch, a ground tow, or neutral air. "Zero sink" means that upward cur a tow by a powered aircraft. Once the sailcraft is rents are just strong enough to enable him to hold airborne and the tow cable released, performance altitude but not to climb. Sailplanes are highly 171 r efficient machines; a sink rate of a mere 2 feet per second. There is no point in trying to soar until second provides an airspeed of about 40 knots, and weather conditions favor vertical speeds greater a sink rate of 6 feet per second gives an airspeed than the minimum sink rate of the aircraft. -
Thesis Characteristics of Hailstorms and Enso
THESIS CHARACTERISTICS OF HAILSTORMS AND ENSO-INDUCED EXTREME STORM VARIABILITY IN SUBTROPICAL SOUTH AMERICA Submitted by Zachary S. Bruick Department of Atmospheric Science In partial fulfillment of the requirements For the Degree of Master of Science Colorado State University Fort Collins, Colorado Spring 2019 Master’s Committee: Advisor: Kristen L. Rasmussen Russ S. Schumacher V. Chandrasekar Copyright by Zachary S. Bruick 2019 All Rights Reserved ABSTRACT CHARACTERISTICS OF HAILSTORMS AND ENSO-INDUCED EXTREME STORM VARIABILITY IN SUBTROPICAL SOUTH AMERICA Convection in subtropical South America is known to be among the strongest anywhere in the world. Severe weather produced from these storms, including hail, strong winds, tornadoes, and flash flooding, causes significant damages to property and agriculture within the region. These in- sights are only due to the novel observations produced by the Tropical Rainfall Measuring Mission (TRMM) satellite since there are the limited ground-based observations within this region. Con- vection is unique in subtropical South America because of the synoptic and orographic processes that support the initiation and maintenance of convection here. Warm and moist air is brought into the region by the South American low-level jet from the Amazon. When the low-level jet intersects the Andean foothills and Sierras de Córdoba, this unstable air is lifted along the orography. At the same time, westerly flow subsides in the lee of the Andes, which provides a capping inversion over the region. When the orographic lift is able to erode the subsidence inversion, convective initiation occurs and strong thunderstorms develop. As a result, convection is most frequent near high terrain. -
Exhibit 18 Ro-6-151
EXHIBIT 18 RO-6-151 1921 University Ave. ▪ Berkeley, CA 94704 ▪ Phone 510-629-4930 ▪ Fax 510-550-2639 Chris Lautenberger [email protected] 12 April 2018 Dan Silver, Executive Director Endangered Habitats League 8424 Santa Monica Blvd., Suite A 592 Los Angeles, CA 90069-4267 Subject: Fire risk impacts of Otay Ranch Village 14 and Planning Areas 16/19 Project Dear Mr. Silver, At your request I have reviewed the Fire Protection Plan (FPP) for the planned Otay Ranch Village 14 and Planning Areas 16/19 Project and analyzed potential fire/life safety impacts of this planned development. Santa Ana winds Santa Ana winds (or Santa Anas for short) present major fire/life safety concerns for the Otay Ranch Village 14 and Planning Areas 16/19 Project. Santa Anas are hot and dry winds that blow through Southern California each year, usually between the months of October and April. Santa Anas occur when high pressure forms in the Great Basin (Western Utah, much of Nevada, and the Eastern border of California) with lower pressure off the coast of Southern California. This pressure gradient drives airflow toward the Pacific Ocean. As air travels West from the Great Basin, orographic lift dries the air as it rises in elevation over mountain ranges. As air descends from high elevations in the Sierra Nevada, its temperature rises dramatically (~5 °F per 1000 ft decrease in elevation). A subsequent drop in relative humidity accompanies this rise in temperature. This drying/heating phenomenon is known as a katabatic wind. Relative humidity in Southern California during Santa Anas is often 10% or lower. -
Influence of Orographic Precipitation on the Co-Evolution of Landforms and Vegetation
EGU2020-5280, updated on 26 Sep 2021 https://doi.org/10.5194/egusphere-egu2020-5280 EGU General Assembly 2020 © Author(s) 2021. This work is distributed under the Creative Commons Attribution 4.0 License. Influence of orographic precipitation on the co-evolution of landforms and vegetation Ankur Srivastava1, Omer Yetemen2, Nikul Kumari1, and Patricia M. Saco1 1University of Newcastle, University of Newcastle, Civil and Environmental Engineering, Callaghan, Australia ([email protected]) 2Eurasia Institute of Earth Sciences, Istanbul Technical University, Istanbul, Turkey Topography plays an important role in controlling the amount and the spatial distribution of precipitation due to orographic lift mechanisms. Thus, it affects the existing climate and vegetation distribution. Recent landscape modelling efforts show how the orographic effects on precipitation result in the development of asymmetric topography. However, these modelling efforts do not include vegetation dynamics that inhibits sediment transport. Here, we use the CHILD landscape evolution model (LEM) coupled with a vegetation dynamics component that explicitly tracks above- and below-ground biomass. We ran the model under three scenarios. A spatially‑uniform precipitation scenario, a scenario with increasing rainfall as a function of elevation, and another one that includes rain shadow effects in which leeward hillslopes receive less rainfall than windward ones. Preliminary results of the model show that competition between increased shear stress due to increased runoff and vegetation protection affects the shape of the catchment. Hillslope asymmetry between polar- and equator-facing hillslopes is enhanced (diminished) when rainfall coincides with a windward (leeward) side of the mountain range. It acts to push the divide (i.e., the boundary between leeward and windward flanks) and leads to basin reorganization through reach capture. -
Literature Review and Scientific Synthesis on the Efficacy of Winter Orographic Cloud Seeding
Statement on the Application of Winter Orographic Cloud Seeding For Water Supply and Energy Production Literature Review and Scientific Synthesis on the Efficacy of Winter Orographic Cloud Seeding A Report to the U.S. Bureau of Reclamation January 2015 Prepared by David W. Reynolds CIRES Boulder, Co 1 Technical Memorandum This information is distributed solely for the purpose of pre-dissemination peer review under applicable information quality guidelines. It has not been formally disseminated by the Bureau of Reclamation. It does not represent and should not be construed to represent Reclamation’s determination or policy. As such, the findings and conclusions in this report are those of the author and do not necessarily represent the views of Reclamation. 2 Statement on the Application of Winter Orographic Cloud Seeding For Water Supply and Energy Production 1.0 Introduction ........................................................................................................................ 5 1.1. Introduction to Winter Orographic Cloud Seeding .......................................................... 5 1.2 Purpose of this Study........................................................................................................ 5 1.3 Relevance and Need for a Reassessment of the Role of Winter Orographic Cloud Seeding to Enhance Water Supplies in the West ........................................................................ 6 1.4 NRC 2003 Report on Critical Issues in Weather Modification – Critical Issues Concerning Winter Orographic -
2019 STAAR Grade 6 Reading Rationales Item# Rationale
2019 STAAR Grade 6 Reading Rationales Item# Rationale 1 Option C is correct A simile is a figure of speech in which two objects are compared using the word “like” or “as.” In line 14, the author contrasts Zach’s normal behavior—“as active as a fly in a doughnut shop”—with his current behavior—“on his stomach sleeping quietly.” The simile is included to help the reader understand how much energy Zach typically has. Option A is incorrect Although the author does contrast Zach sleeping with his normal, active behavior, this is not meant to suggest that Zach has trouble falling asleep. Option B is incorrect The author compares Zach to “a fly in a doughnut shop” to emphasize how much energy Zach typically has; Zach did not actually eat any doughnuts. Option D is incorrect In paragraph 14, the author describes Michelle waking up “earlier than usual” and then taking a picture of her younger brother, so there is no evidence that Zach is sleeping late. 2 Option F is correct The theme of the story is that recognizing an unexpected opportunity can have surprising results. Throughout the story, Michelle is trying to capture the perfect picture of a sunset for the photo contest she has entered. However, she unexpectedly loves the photograph she takes of her sleeping brother and ends up submitting it for the contest. Option G is incorrect Michelle clearly enjoys taking photographs, but she is also interested in winning the photography contest, so this is not the story’s theme. Option H is incorrect Michelle is kind and patient toward her younger brother Zach, but the siblings’ relationship is not a central focus of the story and not significant to the theme. -
Days & Hours for Social Distance Walking Visitor Guidelines Lynden
53 22 D 4 21 8 48 9 38 NORTH 41 3 C 33 34 E 32 46 47 24 45 26 28 14 52 37 12 25 11 19 7 36 20 10 35 2 PARKING 40 39 50 6 5 51 15 17 27 1 44 13 30 18 G 29 16 43 23 PARKING F GARDEN 31 EXIT ENTRANCE BROWN DEER ROAD Lynden Sculpture Garden Visitor Guidelines NO CLIMBING ON SCULPTURE 2145 W. Brown Deer Rd. Do not climb on the sculptures. They are works of art, just as you would find in an indoor art Milwaukee, WI 53217 museum, and are subject to the same issues of deterioration – and they endure the vagaries of our harsh climate. Many of the works have already spent nearly half a century outdoors 414-446-8794 and are quite fragile. Please be gentle with our art. LAKES & POND There is no wading, swimming or fishing allowed in the lakes or pond. Please do not throw For virtual tours of the anything into these bodies of water. VEGETATION & WILDLIFE sculpture collection and Please do not pick our flowers, fruits, or grasses, or climb the trees. We want every visitor to be able to enjoy the same views you have experienced. Protect our wildlife: do not feed, temporary installations, chase or touch fish, ducks, geese, frogs, turtles or other wildlife. visit: lynden.tours WEATHER All visitors must come inside immediately if there is any sign of lightning. PETS Pets are not allowed in the Lynden Sculpture Garden except on designated dog days. -
California Cumulonimbus
California Cumulonimbus Spring 2015 Articles in this Edition: Welcome Message by Jimmy Taeger California CoCoRaHS Regions CoCoRaHS, which stands for Welcome Message 1 lowers are in bloom and the Community Collaborative Rain Northern Mountains F San Joaquin Valley days are getting longer which Hail and Snow network, is a S. Coast - Los Angeles means...it’s time for another edi- group of volunteer observers who S. Coast - San Diego tion of the California Cumulo- report precipitation daily. Not Observer 1 S. Deserts - Vegas Region nimbus! The California Cumulo- only is it fun, but your report Spotlight: Bob SE. Deserts - nimbus is a biannual newsletter gives vital information to organi- Phoenix Region King for California CoCoRaHS ob- zations and individuals such as servers that is issued twice a year; the National Weather Service, once in the spring and once in the River Forecast Centers, farmers, fall. and others. Low Elevation 2 This edition contains articles on Visit cocorahs.org to sign up, or Snow in SoCal the summer climate outlook, an e-mail [email protected] observer spotlight, a low eleva- for additional information. Central Coast tion snow weather event in E. Sierra N. Coast SoCal, the El Niño advisory, the Enjoy the newsletter! Northern Interior continuing California drought California’s 3 and spring in the North Bay area. Summer Climate Map of California divided up into different CoCoRaHS regions. Each Outlook region has one or more coordinators. If you’re not a CoCoRaHS volun- (Source: CoCoRaHS) teer yet, it’s not too late to join! Observer Spotlight: Bob King by Jimmy Taeger El Niño Advisory 3 in Effect of the daily observations, especial- S ince 2009, Bob King has been ly since the gauge was just 20 feet an active and loyal observer to from his bedroom door. -
DYNAMIC SOARING UAV GLIDERS by Jeffrey H. Koessler
Dynamic Soaring UAV Gliders Item Type text; Electronic Dissertation Authors Koessler, Jeffrey H. Publisher The University of Arizona. Rights Copyright © is held by the author. Digital access to this material is made possible by the University Libraries, University of Arizona. Further transmission, reproduction or presentation (such as public display or performance) of protected items is prohibited except with permission of the author. Download date 07/10/2021 13:32:45 Link to Item http://hdl.handle.net/10150/627980 DYNAMIC SOARING UAV GLIDERS by Jeffrey H. Koessler __________________________ Copyright © Jeffrey H. Koessler 2018 A Dissertation Submitted to the Faculty of the DEPARTMENT OF AEROSPACE & MECHANICAL ENGINEERING In Partial Fulfillment of the Requirements For the Degree of DOCTOR OF PHILOSOPHY WITH A MAJOR IN AEROSPACE ENGINEERING In the Graduate College THE UNIVERSITY OF ARIZONA 2018 THEUNIVERSITY OF ARIZONA GRADUATE COLLEGE Date: 01 May 2018 RIZONA 2 STATEMENT BY AUTHOR This dissertation has been submitted in partial fulfillment of the requirements for an advanced degree at the University of Arizona and is deposited in the University Library to be made available to borrowers under rules of the Library. Brief quotations from this dissertation are allowable without special permission, provided that an accurate acknowledgement of the source is made. Requests for permission for extended quotation from or reproduction of this manuscript in whole or in part may be granted by the copyright holder. SIGNED: Jeffrey H. Koessler 3 Acknowledgments This network of mentors, colleagues, friends, and family is simply amazing! Many thanks to... ...My advisor Prof. Fasel for enduring my arguments and crazy ideas about the dynamics of soaring. -
Towards the Improvement of Winter Orographic Cloud Seeding in Utah
TOWARDS THE IMPROVEMENT OF WINTER OROGRAPHIC CLOUD SEEDING IN UTAH Prepared for: Utah Division of Water Resources www. https://water.utah.gov/ Prepared by: The Utah Climate Center December 2019 www.climate.usu.edu Phone: (435) 797-2190 Dr. Binod Pokharel Post-Doctoral Research Scientist, Utah Climate Center Utah State University Prof. Simon Wang, Utah State University & Utah Climate Center Dr. Jon Meyer, Utah Climate Center Dr. Hongping Gu, Utah Climate Center Prof. Matthew LaPlante Utah State University i NOTICE This report was compiled by the Utah Climate Center. The results and conclusions in this report are based on industry-accepted best practices and publicly available data sources. Therefore, neither the Utah Climate Center nor any person acting on behalf of the Utah Climate Center can: (a) make any warranty, expressed or implied, regarding future use of any information or method in this report, or (b) assume any future liability regarding the use of any information or method contained in this report. The funding for this study is provided by the Utah Division of Water Resources, the State of Utah, and the Colorado River Lower Basin States. ii TABLE OF CONTENTS Page TABLE OF CONTENTS .............................................................................................................. iii LIST OF FIGURES ........................................................................................................................v LIST OF TABLES ..................................................................................................................... -
Flight Response of Slope‐Soaring Birds To
Functional Ecology 2014 doi: 10.1111/1365-2435.12381 Flight response of slope-soaring birds to seasonal variation in thermal generation Adam E. Duerr*,1, Tricia A. Miller1, Michael Lanzone2, David Brandes3, Jeff Cooper4, Kieran O’Malley5, Charles Maisonneuve6, Junior A. Tremblay†,7 and Todd Katzner‡,1,8 1Division of Forestry and Natural Resources, West Virginia University, 322 Percival Hall, Morgantown, West Virginia 26506, USA; 2Cellular Tracking Technologies LLC, 2405 North Center Avenue, Suite B, Somerset, Pennsylvania 15501, USA; 3Department of Civil and Environmental Engineering, Acopian Engineering Center, Lafayette College, Easton, Pennsylvania 18042, USA; 4Virginia Department of Game and Inland Fisheries, 1320 Belman Road, 5 Fredericksburg, Virginia 22401, USA; West Virginia Division of Natural Resources, 1 Depot Street, Romney, West 6 Virginia 26575, USA; Ministere du Developpement durable, de l’Environnement, de la Faune et des Parcs, 92, 2e Rue 7 Ouest, Rimouski, Quebec G5L 8B3, Canada; Ministere du Developpement durable, de l’Environnement, de la Faune et des Parcs, 880 chemin Sainte-Foy, Quebec City, Quebec G1S 4X4, Canada; and 8United States Department of Agriculture, Forest Service, Timber and Watershed Laboratory, Parsons, West Virginia 26287, USA Summary 1. Animals respond to a variety of environmental cues, including weather conditions, when migrating. Understanding the relationship between weather and migration behaviour is vital to assessing time- and energy limitations of soaring birds. Different soaring modes have different efficiencies, are dependent upon different types of subsidized lift and are weather dependent. 2. We collected GPS locations from 47 known-age golden eagles that moved along 83 migra- tion tracks. We paired each location with weather to determine meteorological correlates of migration during spring and fall as birds crossed three distinct ecoregions in north-east North America.