A) 50 to 85Km B) 85 to More Than 200Km C) 11 to 50Km D) 0 to 11Km
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Touching the Clouds Activity Guide
Touching the Clouds Activity Guide Purpose Provide a mental representation of each cloud type Create a tactile cloud identification chart Overview Individuals will construct and touch a tactile model of common types of clouds to learn how to describe the clouds based on their shape and texture. They will compare their descriptions with the standard classifications using the cloud types identified in the GLOBE Clouds Protocol. Time: 45 minutes to 1 ½ hours, depending on individual’s age Level: All Materials (per person) One large sheet of cardstock (18” x 12”) Tape One set of Braille labels for each cloud type and/or markers One small feather A layered piece of blanket or soft fabric (eight 1’ X 1” pieces) Cotton balls of varied sizes One tissue Organza or a similar material, cut into pieces, one layered 1” x 1” piece Pillow stuffing, one 1” x 1” piece A tsp of sand Three paper clips Liquid glue Scissors Baby Wipes Preparation Use tape to divide the large cardstock sheet in four sections: one for the cloud title at the top and three for the altitudes: using a portrait layout, place three pieces of tape horizontally, from side to side of the sheet. 1. 1” off the upper edge of the sheet 2. 8” off the upper edge of the sheet 1 Steps What to do and how to do it: Making A Tactile Cloud Identification Chart 1. Discuss that clouds come in three basic shapes: cirrus, stratus and cumulus. a. Feel of the 4” feather and describe it; discuss that these wispy clouds are high in the sky and are named cirrus. -
Tides Foundation 2017 Form
OMB No. 1545-0047 Form 990 Return of Organization Exempt From Income Tax 2017 Under section 501(c), 527, or 4947(a)(1) of the Internal Revenue Code (except private foundations) G Do not enter social security numbers on this form as it may be made public. Open to Public Department of the Treasury Internal Revenue Service G Go to www.irs.gov/Form990 for instructions and the latest information. Inspection A For the 2017 calendar year, or tax year beginning , 2017, and ending , B Check if applicable: C D Employer identification number Address change Tides Foundation 51-0198509 Name change P.O. Box 29903 E Telephone number Initial return San Francisco, CA 94129-0903 415-561-6400 Final return/terminated X Amended return G Gross receipts $ 439,417,675. Application pending F Name and address of principal officer: Kriss Deiglmeier H(a) Is this a group return for subordinates? Yes X No H(b) Are all subordinates included? Yes No Same As C Above If 'No,' attach a list. (see instructions) I Tax-exempt status X 501(c)(3) 501(c) ( )H (insert no.) 4947(a)(1) or 527 J Website: G www.tides.org H(c) Group exemption number G K Form of organization: X Corporation Trust Association OtherG L Year of formation: 1976 M State of legal domicile: CA Part I Summary 1 Briefly describe the organization's mission or most significant activities:Tides Foundation's primary exempt purpose is grantmaking. We empower individuals and institutions to move money efficiently and effectively towards positive social change. 2 Check this box G if the organization discontinued its operations or disposed of more than 25% of its net assets. -
Graphical Area Forecast User Guide a Guide for the Transition from Arfors to GAF
Graphical Area Forecast User Guide A guide for the transition from ARFORs to GAF October 2017 | Version 1.2 Graphical Area Forecast User Guide Document Control Revision history VERSION DATE DESCRIPTION AUTHOR 1 15 September 2017 Final version Elizabeth Heba Update to provide clarification on AIRMETs 1.1 13 October 2017 Elizabeth Heba and SIGMETs Update to GAF samples and worked example 1.2 20 October 2017 Additional text in Area Briefing (NAIPS) Ashwin Naidu Section Update to abbreviation examples Approval for release DATE NAME Position Signature National Manager Aviation 20 October 2017 Gordon Jackson Meteorological Services Version number Date of issue th Version 1.2 20 October 2017 © Commonwealth of Australia 2017 This work is copyright. Apart from any use as permitted under the Copyright Act 1968, no part may be reproduced without prior written permission from the Bureau of Meteorology. Requests and inquiries concerning reproduction and rights should be addressed to the Production Manager, Communication Section, Bureau of Meteorology, GPO Box 1289, Melbourne 3001. Information regarding requests for reproduction of material from the Bureau website can be found at www.bom.gov.au/other/copyright.shtml ii Graphical Area Forecast User Guide Table of Contents 1 Purpose .......................................................................................................................................... 1 2 Introduction ................................................................................................................................... -
Types of Clouds
Types of Clouds What’s the Weather? Cirrus, Cirrocumulus and Cirrostratus (high 5000-16,000 m) . thin and often wispy . composed of ice crystals that originate from the freezing of supercooled water droplets. Generally occur in fair weather and point in the direction of air movement at their elevation. Cirrus . They are made of ice crystals and have long, thin, wispy streamers. Cirrus clouds are usually white and predict fair weather. cirrus cirrus cirrus cirrus cirrus cirrus Cirrocumulus . They are small rounded puffs that usually appear in long rows. Cirrocumulus are usually white, but sometimes appear gray. Cirrocumulus are usually seen in the winter time and mean that there will be fair, but cold weather. Cirrostratus . Sheetlike thin clouds that usually cover the entire sky. Cirrostratus clouds usually come 12-24 hours before a rain or snow storm. Altocumulus and Altostratus (middle 2,000 to 7, 000 m) . Middle clouds are made of ice crystals and water droplets. The base of a middle cloud above the surface can be anywhere from 2000-8000m in the tropics to 2000-4000m in the polar regions. An Altocumulus . They are grayish-white with one part of the cloud darker than the other. Usually form in groups. If you see altocumulus clouds on a warm sticky morning, then expect thunderstorms by late afternoon. Altostratus . An altostratus cloud usually covers the whole sky. The cloud looks gray or blue-gray. Usually forms ahead of storms that have a lot of rain or snow. Sometimes, rain will fall from an altostratus cloud. If the rain hits the ground, then the cloud is called a nimbostratus cloud. -
ICA Vol. 1 (1956 Edition)
·wMo o '-" I q Sb 10 c. v. i. J c.. A INTERNATIONAL CLOUD ATLAS Volume I WORLD METEOROLOGICAL ORGANIZATION 1956 c....._/ O,-/ - 1~ L ) I TABLE OF CONTENTS Pages Preface to the 1939 edition . IX Preface to the present edition . xv PART I - CLOUDS CHAPTER I Introduction 1. Definition of a cloud . 3 2. Appearance of clouds . 3 (1) Luminance . 3 (2) Colour .... 4 3. Classification of clouds 5 (1) Genera . 5 (2) Species . 5 (3) Varieties . 5 ( 4) Supplementary features and accessory clouds 6 (5) Mother-clouds . 6 4. Table of classification of clouds . 7 5. Table of abbreviations and symbols of clouds . 8 CHAPTER II Definitions I. Some useful concepts . 9 (1) Height, altitude, vertical extent 9 (2) Etages .... .... 9 2. Observational conditions to which definitions of clouds apply. 10 3. Definitions of clouds 10 (1) Genera . 10 (2) Species . 11 (3) Varieties 14 (4) Supplementary features and accessory clouds 16 CHAPTER III Descriptions of clouds 1. Cirrus . .. 19 2. Cirrocumulus . 21 3. Cirrostratus 23 4. Altocumulus . 25 5. Altostratus . 28 6. Nimbostratus . 30 " IV TABLE OF CONTENTS Pages 7. Stratoculllulus 32 8. Stratus 35 9. Culllulus . 37 10. Culllulonimbus 40 CHAPTER IV Orographic influences 1. Occurrence, structure and shapes of orographic clouds . 43 2. Changes in the shape and structure of clouds due to orographic influences 44 CHAPTER V Clouds as seen from aircraft 1. Special problellls involved . 45 (1) Differences between the observation of clouds frolll aircraft and frolll the earth's surface . 45 (2) Field of vision . 45 (3) Appearance of clouds. 45 (4) Icing . -
Degradation of Radar Reflectivity by Cloud Attenuation at Microwave Frequency
640 JOURNAL OF ATMOSPHERIC AND OCEANIC TECHNOLOGY VOLUME 24 Degradation of Radar Reflectivity by Cloud Attenuation at Microwave Frequency OLIVIER PUJOL AND JEAN-FRANÇOIS GEORGIS Laboratoire d’Aérologie, Observatoire Midi-Pyrénées, Université Paul Sabatier, Toulouse, France LAURENT FÉRAL Laboratoire AD2M, Université Paul Sabatier, Toulouse, France HENRI SAUVAGEOT Laboratoire d’Aérologie, Observatoire Midi-Pyrénées, Université Paul Sabatier, Toulouse, France (Manuscript received 2 November 2005, in final form 7 June 2006) ABSTRACT The main object of this paper is to emphasize that clouds—the nonprecipitating component of condensed atmospheric water—can produce a strong attenuation at operational microwave frequencies, although they present a low reflectivity preventing their radar detection. By way of a simple and realistic model, simu- lations of radar observations through warm precipitating targets are thus presented in order to quantify cloud attenuation. Simulations concern an airborne radar oriented downward and observing precipitation at four frequencies: 3, 10, 35, and 94 GHz. Two cases are first considered: a convective cell (vigorous cumulus congestus plus rain) and a stratiform one (nimbostratus plus drizzle) superimposed on the previous one. Other simulations are then performed on different types of cumulus (congestus, mediocris, and hu- milis) with various thicknesses characterized, in a microphysical sense, by their maximum liquid water content. Simulations confirm the low cumulus reflectivity ranging from Ϫ45 dBZ for the weakest cumulus (i.e., the humilis one) to Ϫ5dBZ for the strongest one (i.e., the vigorous cumulus congestus). It reaches Ϫ35 dBZ for the nimbostratus cloud. On the other hand, cumulus attenuation [precisely path-integrated cloud at- tenuation (PICA)] is not negligible and, depending on the frequency, can be very strong: the higher the frequency, the stronger the PICA. -
Glossary of Clouds Weather Terms
SkyStef's weather page home | e-mail Glossary of terms for clouds Definition of a cloud: a hydrometeor consisting of minute particles of liquid water or ice, or of both, suspended in the free air and usually not touching the ground. It may also include larger particles of liquid water or ice as well as non-aqueous or solid particles such as those present in fumes, smoke or dust. Principles of cloud classification: clouds are continuously in a process of evolution and appear, therefore, in a infinite variety of forms. It is possible, however, to define a limited number of characteristic forms, frequently observed all over the world, into which clouds can be broadly grouped. A classification of the characteristic forms of clouds, in terms of "genera", "species", and "varieties" has been established. Definitions and descriptions of each of the characteristic forms corresponding to this classification are given in the list below. Intermediate or transitional forms, although observed fairly frequently, are not described; they are of little intrest, as they are less stable and as their appearance is not very different from that indicated in the definitions of the characteristic forms. Finally, there exists a group of clouds, rarely or occassionally observed, not included in this classification. Some of these so called "special clouds" consists for the greater part or in their entirety of non- aqueous liquid or solid particles. The above mentioned definition of a cloud is therefore not applicable to all special clouds. Special clouds are: nacreous clouds, noctilucent clouds, condensation trails, clouds from waterfalls, clouds from fires, clouds from volcanic eruptions, clouds resulting from industry and clouds resulting from explosions. -
Citizen Inquiry: Engaging Citizens in Online Communities of Scientific Inquiries
Open Research Online The Open University’s repository of research publications and other research outputs Citizen Inquiry: Engaging Citizens in Online Communities of Scientific Inquiries Thesis How to cite: Aristeidou, Maria (2016). Citizen Inquiry: Engaging Citizens in Online Communities of Scientific Inquiries. PhD thesis Institute of Educational Technology. For guidance on citations see FAQs. c [not recorded] https://creativecommons.org/licenses/by-nc-nd/4.0/ Version: Version of Record Copyright and Moral Rights for the articles on this site are retained by the individual authors and/or other copyright owners. For more information on Open Research Online’s data policy on reuse of materials please consult the policies page. oro.open.ac.uk Citizen Inquiry: Engaging Citizens in Online Communities of Scientific Inquiries Maria Aristeidou BA Education Science and Primary Education MSc Technology Education and Digital Systems (e-Learning) Submitted for the degree of Doctor of Philosophy Institute of Educational Technology The Open University March 2016 1 Abstract Citizen Inquiry has been proposed as an informal science learning approach to enable widespread involvement in science and empower citizens with reasoning and problem-solving skills used by scientists. It combines aspects from citizen science and inquiry-based learning, producing science learning experiences within distributed communities of interest. A central challenge for Citizen Inquiry is to involve citizens in planning and implementing their own investigations, supported and guided by online systems and tools within an inquiry environment, while collaborating with science experts and non-experts. This thesis explores how to create an active and sustainable online community for citizens to engage in scientific investigations. -
The Ten Different Types of Clouds
THE COMPLETE GUIDE TO THE TEN DIFFERENT TYPES OF CLOUDS AND HOW TO IDENTIFY THEM Dedicated to those who are passionately curious, keep their heads in the clouds, and keep their eyes on the skies. And to Luke Howard, the father of cloud classification. 4 Infographic 5 Introduction 12 Cirrus 18 Cirrocumulus 25 Cirrostratus 31 Altocumulus 38 Altostratus 45 Nimbostratus TABLE OF CONTENTS TABLE 51 Cumulonimbus 57 Cumulus 64 Stratus 71 Stratocumulus 79 Our Mission 80 Extras Cloud Types: An Infographic 4 An Introduction to the 10 Different An Introduction to the 10 Different Types of Clouds Types of Clouds ⛅ Clouds are the equivalent of an ever-evolving painting in the sky. They have the ability to make for magnificent sunrises and spectacular sunsets. We’re surrounded by clouds almost every day of our lives. Let’s take the time and learn a little bit more about them! The following information is presented to you as a comprehensive guide to the ten different types of clouds and how to idenify them. Let’s just say it’s an instruction manual to the sky. Here you’ll learn about the ten different cloud types: their characteristics, how they differentiate from the other cloud types, and much more. So three cheers to you for starting on your cloud identification journey. Happy cloudspotting, friends! The Three High Level Clouds Cirrus (Ci) Cirrocumulus (Cc) Cirrostratus (Cs) High, wispy streaks High-altitude cloudlets Pale, veil-like layer High-altitude, thin, and wispy cloud High-altitude, thin, and wispy cloud streaks made of ice crystals streaks -
Climatology Climatic Zone
Climatology Climatic Zone 1320. At about what geographical latitude as average is assumed for the zone of prevailing westerlies? A) 10° N. B) 50° N. C) 80° N. D) 30° N. 1321. What is the type, intensity and seasonal variation of precipitation in the equatorial region? A) Rain showers, hail showers and thunderstorms occur the whole year, but frequency is highest during two periods: April-May and October- November. B) Precipitation is generally in the form of showers but continuous rain occurs also. The greatest intensity is in July. C) Warm fronts are common with continuous rain. The frequency is the same throughout the year D) Showers of rain or hail occur throughout the year; the frequency is highest in January. 1324. The reason for the fact, that the Icelandic low is normally deeper in winter than in summer is that: A) the strong winds of the north Atlantic in winter are favourable for the development of lows. B) the low pressure activity of the sea east of Canada is higher in winter. C) the temperature contrasts between arctic and equatorial areas are much greater in winter. D) converging air currents are of greater intensity in winter. 1328. The lowest relative humidity will be found: A) at the south pole. B) between latitudes 30 deg and 40 deg N in July. C) in equatorial regions. D) around 30 deg S in January. Tropical Climatology: 1329. Flying from Dakar to Rio de Janeiro in winter where would you cross the ITCZ? A) 7 to 120N. B) 0 to 70N. C) 7 to 120S. -
The Kiwi Kids Cloud Identification Guide
Droplets The Kiwi Kids Cloud Identification Guide Written by Paula McKean Droplets The Kiwi Kids Cloud Identification Guide ISBN 1-877264-27-X Paula McKean MEd Hons (Science Ed), BEd, DipTchg 2009 © Crown Copyright 2009 Contents 1. Cloud Classification 2. How Clouds are formed 3. The Water Cycle 4. Cumulus Altitudes 5. Stratus Altitudes 6. Precipitating Cloud Altitudes 7. Cirrus Cloud Altitudes 8. Cumulus 10. Altocumulus 12. Cirrocumulus 14. Stratus 16. Stratocumulus 18. Altostratus 20. Cirrostratus 22. Nimbostratus 24. Cumulus Congestus 26. Cumulonimbus 28. Cirrus 30. Contrails 32. References 33. Acknowledgements Cloud Classification Since Luke Howard developed the first cloud classification system in 1802, clouds have been classified according to the altitude of the cloud base and the shape of the cloud. There are three main categories: Low level- Clouds that form below 2000 m: Cumulus, Stratocumulus, Stratus (including Fog, Haze and Mist), Nimbostratus and Cumulonimbus. Mid level - Clouds that form between 2000 m and 7000 m: Altocumulus and Altostratus. High level - Clouds that form above 5000 m: Cirrus, Cirrocumulus, Cirrostratus and Contrails. In this guide cloud types have been organised by their characteristics so it is easier to distinguish between clouds that appear to be similar and to help determine the cloud type when the altitude can’t be determined. Clouds have been grouped into four categories: • Cumulus (heaped, puffy appearing clouds). • Stratus (flat clouds that extend over large sections of sky). • Precipitating (clouds that can produce rain, hail or snow). • Cirrus (wispy high altitude clouds). By using a combination of the altitude system and characteristic based system used in this guide, cloud identification will be easier and more accurate. -
Use of Spatial Technologies to Study the Winds' Directions in Rub' Al
Journal of Earth Science and Engineering 5 (2015) 372-381 doi: 10.17265/2159-581X/2015.06.005 D DAVID PUBLISHING Use of Spatial Technologies to Study the Winds’ Directions in Rub’ Al-Khali Desert, Saudi Arabia Ali Madan Al-Ali Albab for Environmental and Geo-Informatics Studies, P. O. Box 899, Saihat 31972, Eastern Province, Saudi Arabia Abstract: Studying environmental phenomenon in Rub’ Al-Khali (Arabic name of “Empty Quarter”), as one of the largest deserts in the world, requires adopting some advanced spatial technologies in conjunction with the data recorded in the field in order to device better understanding. The paper utilizes the technologies of GIS (geographical information systems) and RS (remote sensing) in order to study large amount of weather data recorded in the field from different sources related to oil and gas industry in Rub’ Al-Khali desert. The main objective is to identify the wind directions and its movement in Kidan areas and the areas south and east of Shaybah in Rub’ Al-Khali desert. The study used different sources of data mainly recorded by the seismic campaigns’ base camps and the drilling rig camps or the civil works camps. Wind Roses were created for all metrological weather stations in the study area. Also, the study tried to analyze the dune types using satellite imageries and identify the relation of its shapes to the wind direction. The final aim of the result of this study is to help in planning best locations to build facilities for new major oil and gas project. Key words: Wind, oil, directions, roses, GIS.