Oklahoma Climate
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University of Oklahoma
UNIVERSITY OF OKLAHOMA GRADUATE COLLEGE INVESTIGATION OF POLARIMETRIC MEASUREMENTS OF RAINFALL AT CLOSE AND DISTANT RANGES A DISSERTATION SUBMITTED TO THE GRADUATE FACULTY in partial fulfillment of the requirements for the degree of Doctor of Philosophy By SCOTT EDWARD GIANGRANDE Norman, Oklahoma 2007 UMI Number: 3291249 UMI Microform 3291249 Copyright 2008 by ProQuest Information and Learning Company. All rights reserved. This microform edition is protected against unauthorized copying under Title 17, United States Code. ProQuest Information and Learning Company 300 North Zeeb Road P.O. Box 1346 Ann Arbor, MI 48106-1346 INVESTIGATION OF POLARIMETRIC MEASUREMENTS OF RAINFALL AT CLOSE AND DISTANT RANGES A DISSERTATION APPROVED FOR THE SCHOOL OF METEOROLOGY BY ____________________________________ Dr. Michael Biggerstaff ____________________________________ Dr. Alexander Ryzhkov ____________________________________ Dr. Jerry Straka ____________________________________ Dr. Guifu Zhang ____________________________________ Dr. Mark Yeary © Copyright by SCOTT EDWARD GIANGRANDE 2007 All Rights Reserved. ACKNOWLEDGEMENTS I would like to extend my sincerest thanks to the numerous individuals who have helped me complete this work. To begin, this work would not have been possible without the guidance of my primary research advisor, Dr. Alexander Ryzhkov. His leadership and patience were instrumental throughout this process. I would also like to extend my gratitude to the other members of my committee: Drs. Michael Biggerstaff (Co-Chair and primary OU School of Meteorology advisor), Guifu Zhang, Jerry Straka, and Mark Yeary. The reviews performed by these individuals strengthened this work. I also thank the members of the Radar Research and Development Division (RRDD) at the National Severe Storms Laboratory (NSSL), which includes Drs. Douglas Forsyth, Dusan Zrnic, Dick Doviak, Allen Zahrai, Terry Schuur, Pam Heinselman, Valery Melnikov, Sebastian Torres, Pengfei Zhang and Svetlana Bachmann. -
Weather Charts Natural History Museum of Utah – Nature Unleashed Stefan Brems
Weather Charts Natural History Museum of Utah – Nature Unleashed Stefan Brems Across the world, many different charts of different formats are used by different governments. These charts can be anything from a simple prognostic chart, used to convey weather forecasts in a simple to read visual manner to the much more complex Wind and Temperature charts used by meteorologists and pilots to determine current and forecast weather conditions at high altitudes. When used properly these charts can be the key to accurately determining the weather conditions in the near future. This Write-Up will provide a brief introduction to several common types of charts. Prognostic Charts To the untrained eye, this chart looks like a strange piece of modern art that an angry mathematician scribbled numbers on. However, this chart is an extremely important resource when evaluating the movement of weather fronts and pressure areas. Fronts Depicted on the chart are weather front combined into four categories; Warm Fronts, Cold Fronts, Stationary Fronts and Occluded Fronts. Warm fronts are depicted by red line with red semi-circles covering one edge. The front movement is indicated by the direction the semi- circles are pointing. The front follows the Semi-Circles. Since the example above has the semi-circles on the top, the front would be indicated as moving up. Cold fronts are depicted as a blue line with blue triangles along one side. Like warm fronts, the direction in which the blue triangles are pointing dictates the direction of the cold front. Stationary fronts are frontal systems which have stalled and are no longer moving. -
NWS Unified Surface Analysis Manual
Unified Surface Analysis Manual Weather Prediction Center Ocean Prediction Center National Hurricane Center Honolulu Forecast Office November 21, 2013 Table of Contents Chapter 1: Surface Analysis – Its History at the Analysis Centers…………….3 Chapter 2: Datasets available for creation of the Unified Analysis………...…..5 Chapter 3: The Unified Surface Analysis and related features.……….……….19 Chapter 4: Creation/Merging of the Unified Surface Analysis………….……..24 Chapter 5: Bibliography………………………………………………….…….30 Appendix A: Unified Graphics Legend showing Ocean Center symbols.….…33 2 Chapter 1: Surface Analysis – Its History at the Analysis Centers 1. INTRODUCTION Since 1942, surface analyses produced by several different offices within the U.S. Weather Bureau (USWB) and the National Oceanic and Atmospheric Administration’s (NOAA’s) National Weather Service (NWS) were generally based on the Norwegian Cyclone Model (Bjerknes 1919) over land, and in recent decades, the Shapiro-Keyser Model over the mid-latitudes of the ocean. The graphic below shows a typical evolution according to both models of cyclone development. Conceptual models of cyclone evolution showing lower-tropospheric (e.g., 850-hPa) geopotential height and fronts (top), and lower-tropospheric potential temperature (bottom). (a) Norwegian cyclone model: (I) incipient frontal cyclone, (II) and (III) narrowing warm sector, (IV) occlusion; (b) Shapiro–Keyser cyclone model: (I) incipient frontal cyclone, (II) frontal fracture, (III) frontal T-bone and bent-back front, (IV) frontal T-bone and warm seclusion. Panel (b) is adapted from Shapiro and Keyser (1990) , their FIG. 10.27 ) to enhance the zonal elongation of the cyclone and fronts and to reflect the continued existence of the frontal T-bone in stage IV. -
WINTER 1998 TH In*Vi'i§
a i 9dardy'fernSFoundationm Editor Sue Olsen VOLUME 7 NUMBER 1 WINTER 1998 TH in*vi'i§ Presidents’ Message: More Inside... Jocelyn Horder and Anne Holt, Co-Presidents Polypodium polypodioides.2 Greetings and best wishes for a wonderful fern filled 1998. At this winter time of year Deer Problems.2 many of our hardy ferns offer a welcome evergreen touch to the garden. The varied textures are particularly welcome in bare areas. Meanwhile ferns make wonderful Book Review.3 companions to your early spring flowering bulbs and blooming plants. Since we are Exploring Private having (so far) a mild winter continue to control the slugs and snails that are lurking European Gardens Continued.4 around your ferns and other delicacies. Mr. Gassner Writes.5 Don’t forget to come to the Northwest Flower and Garden show February 4-8 to enjoy Notes from the Editor.5 the colors, fragrances and fun of spring. The Hardy Fern Foundation will have a dis¬ play of ferns in connection with the Rhododendron Species Botanical Garden. Look for Fem Gardens of the Past and a Garden in Progress.6-7 booth #6117-9 on the fourth floor of the Convention Center where we will have a dis¬ play of ferns, list of fern sources, cultural information and as always persons ready to Fem Finding in the Hocking Hills.8-10 answer your questions. Anyone interested in becoming more involved with the Hardy Blechnum Penna-Marina Fern Foundation will have a chance to sign up for volunteering in the future. Little Hard Fem.10 We are happy to welcome the Coastal Botanical Garden in Maine as a new satellite The 1997 HFF garden. -
December 2013
Oklahoma Monthly Climate Summary DECEMBER 2013 A frigid and sometimes icy December seemed a fitting way to 1.53 inches, about a half-inch below normal, to rank as the close out the boisterous weather of 2013. Preliminary data from 59th wettest December on record. That total is possibly an the Oklahoma Mesonet ranked the month as the 17th coolest underestimate due to the frozen precipitation, although the December on record at nearly 4 degrees below normal. Records moisture pattern across various parts of the state was quite of this type for Oklahoma date back to 1895. The statewide clear. Far southeastern Oklahoma received from 3-5 inches average temperature as recorded by the Mesonet was 35.2 during the month while western areas of the state received degrees. As chilly as it seemed, however, that mark provided less than a half-inch, in general. little threat to 1983’s record cold of 25.8 degrees, but also far cooler than 2012’s 42.1 degrees. There were two significant The cold December propelled 2013’s statewide average winter storms during December, each creating headaches for annual temperature to a mark of 58.9 degrees, 0.8 degrees travelers and power utility companies. The first storm struck on below normal and the 27th coolest calendar year on record for December 5-6 in two separate waves and brought freezing rain, the state. That mark stands in stark contrast to 2012’s record sleet and snow across the state. Significant snow totals of 5-6 warm year of 63.1 degrees. -
Ten Years of Winter: the Cold Decade and Environmental
TEN YEARS OF WINTER: THE COLD DECADE AND ENVIRONMENTAL CONSCIOUSNESS IN THE EARLY 19 TH CENTURY by MICHAEL SEAN MUNGER A DISSERTATION Presented to the Department of History and the Graduate School of the University of Oregon in partial fulfillment of the requirements for the degree of Doctor of Philosophy June 2017 DISSERTATION APPROVAL PAGE Student: Michael Sean Munger Title: Ten Years of Winter: The Cold Decade and Environmental Consciousness in the Early 19 th Century This dissertation has been accepted and approved in partial fulfillment of the requirements for the Doctor of Philosophy degree in the Department of History by: Matthew Dennis Chair Lindsay Braun Core Member Marsha Weisiger Core Member Mark Carey Institutional Representative and Scott L. Pratt Dean of the Graduate School Original approval signatures are on file with the University of Oregon Graduate School. Degree awarded June 2017 ii © 2017 Michael Sean Munger iii DISSERTATION ABSTRACT Michael Sean Munger Doctor of Philosophy Department of History June 2017 Title: Ten Years of Winter: The Cold Decade and Environmental Consciousness in the Early 19 th Century Two volcanic eruptions in 1809 and 1815 shrouded the earth in sulfur dioxide and triggered a series of weather and climate anomalies manifesting themselves between 1810 and 1819, a period that scientists have termed the “Cold Decade.” People who lived during the Cold Decade appreciated its anomalies through direct experience, and they employed a number of cognitive and analytical tools to try to construct the environmental worlds in which they lived. Environmental consciousness in the early 19 th century commonly operated on two interrelated layers. -
ESSENTIALS of METEOROLOGY (7Th Ed.) GLOSSARY
ESSENTIALS OF METEOROLOGY (7th ed.) GLOSSARY Chapter 1 Aerosols Tiny suspended solid particles (dust, smoke, etc.) or liquid droplets that enter the atmosphere from either natural or human (anthropogenic) sources, such as the burning of fossil fuels. Sulfur-containing fossil fuels, such as coal, produce sulfate aerosols. Air density The ratio of the mass of a substance to the volume occupied by it. Air density is usually expressed as g/cm3 or kg/m3. Also See Density. Air pressure The pressure exerted by the mass of air above a given point, usually expressed in millibars (mb), inches of (atmospheric mercury (Hg) or in hectopascals (hPa). pressure) Atmosphere The envelope of gases that surround a planet and are held to it by the planet's gravitational attraction. The earth's atmosphere is mainly nitrogen and oxygen. Carbon dioxide (CO2) A colorless, odorless gas whose concentration is about 0.039 percent (390 ppm) in a volume of air near sea level. It is a selective absorber of infrared radiation and, consequently, it is important in the earth's atmospheric greenhouse effect. Solid CO2 is called dry ice. Climate The accumulation of daily and seasonal weather events over a long period of time. Front The transition zone between two distinct air masses. Hurricane A tropical cyclone having winds in excess of 64 knots (74 mi/hr). Ionosphere An electrified region of the upper atmosphere where fairly large concentrations of ions and free electrons exist. Lapse rate The rate at which an atmospheric variable (usually temperature) decreases with height. (See Environmental lapse rate.) Mesosphere The atmospheric layer between the stratosphere and the thermosphere. -
Surface Station Model (U.S.)
Surface Station Model (U.S.) Notes: Pressure Leading 10 or 9 is not plotted for surface pressure Greater than 500 = 950 to 999 mb Less than 500 = 1000 to 1050 mb 988 Æ 998.8 mb 200 Æ 1020.0 mb Sky Cover, Weather Symbols on a Surface Station Model Wind Speed How to read: Half barb = 5 knots Full barb = 10 knots Flag = 50 knots 1 knot = 1 nautical mile per hour = 1.15 mph = 65 knots The direction of the Wind direction barb reflects which way the wind is coming from NORTHERLY From the north 360° 270° 90° 180° WESTERLY EASTERLY From the west From the east SOUTHERLY From the south Four types of fronts COLD FRONT: Cold air overtakes warm air. B to C WARM FRONT: Warm air overtakes cold air. C to D OCCLUDED FRONT: Cold air catches up to the warm front. C to Low pressure center STATIONARY FRONT: No movement of air masses. A to B Fronts and Extratropical Cyclones Feb. 24, 2007 Case In mid-latitudes, fronts are part of the structure of extratropical cyclones. Extratropical cyclones form because of the horizontal temperature gradient and are part of the general circulation—helping to transport energy from equator to pole. Type of weather and air masses in relation to fronts: Feb. 24, 2007 case mPmP cPcP mTmT Characteristics of a front 1. Sharp temperature changes over a short distance 2. Changes in moisture content 3. Wind shifts 4. A lowering of surface pressure, or pressure trough 5. Clouds and precipitation We’ll see how these characteristics manifest themselves for fronts in North America using the example from Feb. -
“Little Tibet” with “Little Mecca”: Religion, Ethnicity and Social Change on the Sino-Tibetan Borderland (China)
“LITTLE TIBET” WITH “LITTLE MECCA”: RELIGION, ETHNICITY AND SOCIAL CHANGE ON THE SINO-TIBETAN BORDERLAND (CHINA) A Dissertation Presented to the Faculty of the Graduate School of Cornell University In Partial Fulfillment of the Requirements for the Degree of Doctor of Philosophy by Yinong Zhang August 2009 © 2009 Yinong Zhang “LITTLE TIBET” WITH “LITTLE MECCA”: RELIGION, ETHNICITY AND SOCIAL CHANGE ON THE SINO-TIBETAN BORDERLAND (CHINA) Yinong Zhang, Ph. D. Cornell University 2009 This dissertation examines the complexity of religious and ethnic diversity in the context of contemporary China. Based on my two years of ethnographic fieldwork in Taktsang Lhamo (Ch: Langmusi) of southern Gansu province, I investigate the ethnic and religious revival since the Chinese political relaxation in the 1980s in two local communities: one is the salient Tibetan Buddhist revival represented by the rebuilding of the local monastery, the revitalization of religious and folk ceremonies, and the rising attention from the tourists; the other is the almost invisible Islamic revival among the Chinese Muslims (Hui) who have inhabited in this Tibetan land for centuries. Distinctive when compared to their Tibetan counterpart, the most noticeable phenomenon in the local Hui revival is a revitalization of Hui entrepreneurship, which is represented by the dominant Hui restaurants, shops, hotels, and bus lines. As I show in my dissertation both the Tibetan monastic ceremonies and Hui entrepreneurship are the intrinsic part of local ethnoreligious revival. Moreover these seemingly unrelated phenomena are in fact closely related and reflect the modern Chinese nation-building as well as the influences from an increasingly globalized and government directed Chinese market. -
You Are a Meterologist!
YOU ARE A METEROLOGIST! ★A meteorologist is a scientist who studies the atmosphere to forecast weather in a given area. ASSIGNMENT: You have been hired by the Weather Channel as a meteorologist to forecast weather in the United States. Since the Weather Channel provides forecasts for all over the country, your first assignment with them is to forecast four different areas of the United States using your knowledge about air masses and fronts. TASK: 1.) Examine the map of the United States and locate the four cities named on your data table. (Use an atlas to help you find these places.) 2.) After locating the cities, identify and describe the fronts heading towards each city and the air mass that follows it. (Use your reference sheet to help recall types of air mass: continental polar, continental tropical, maritime polar, or maritime tropical.) Record this information in the data table. 3.) For each city, predict how the incoming front will change the weather (temperature, air pressure, storms in that area.) Record your thinking in the data table. 4.) Select one city and write a paragraph about the anticipated weather for that area. Be sure to include data from the table to explain your thinking and forecast. DATA TABLE-FORECASTING WEATHER IN THE UNITED STATES INCOMING INCOMING CITY, STATE FRONT AIR MASS EXPLAIN HOW THIS FRONT MIGHT CHANGE THE IN THE UNITED (Warm Front How do you know? WEATHER AT THIS AREA? STATES or Cold Front) (What’s your evidence from the map?) TEMPERATURE POSSIBLE WEATHER St. Louis, Missouri El Paso, Texas Atlanta, Georgia Minneapolis Minnesota ★MAKE AN INFERENCE: Locate Boston, Massachusetts. -
Weatherscope Weatherscope Application Information: Weatherscope Is a Stand-Alone Application That Makes Viewing Weather Data Easier
User Guide - Macintosh http://earthstorm.ocs.ou.edu WeatherScope WeatherScope Application Information: WeatherScope is a stand-alone application that makes viewing weather data easier. To run WeatherScope, Mac OS X version 10.3.7, a minimum of 512MB of RAM, and an accelerated graphics card with 32MB of VRAM are required. WeatherScope is distributed freely for noncommercial and educational use and can be used on both Apple Macintosh and Windows operating systems. How do I Download WeatherScope? To download the application, go to http://earthstorm.ocs.ou.edu, select Data, Software, Download, or go to http://www. ocs.ou.edu/software. There will be three options: WeatherBuddy, WeatherScope, and WxScope Plugin. You will want to choose WeatherScope. There are two options under the application: Macintosh or Windows. Choose Macintosh to download the application. The installation wizard will automatically save to your desktop. Go to your desktop and double click on the icon that says WeatherScope- x.x.x.pkg. Several dialog messages will appear. The fi rst message will inform you that you are about to install the application. The next message tells you about computer system requirements in order to download the application. The following message is the Software License Agreement. It is strongly suggested that you read this agreement. If you agree, click Agree. If you do not agree, click Disagree and the software will not be installed onto your computer. The next message asks you to select a destination drive (usually your hard drive). The setup will run and install the software on your computer. You may then press Close. -
Winter Weather Awareness Day 2010
Nebraska Winter Weather Awareness Day Winter Weather Awareness Day - November 4, 2010 With Fall upon the Great Plains, now is the time to focus attention to winter weather and the dangers it can pose to life and property. November 4th, 2010 has been declared as Winter Weather Awareness Day for the state of Nebraska. Each year, dozens of Americans die due to exposure to the cold. Winter weather accounts for vehicle accidents and fatalities, and results in fires due to dangerous use of heaters and other winter weather fatalities. Other hazards, such as hypothermia and frostbite, can lead to the loss of fingers and toes or cause permanent internal injuries and even death. The very young and the elderly are among those most vulnerable to the potentially harsh winter conditions. Recognizing the threats and knowing what to do when they occur could prevent the loss of extremities or save a life. A winter storm can last for several days and be accompanied by high winds, freezing rain or sleet, heavy snowfall and cold temperatures. People can be trapped at home or in a car with no utilities or assistance, and those who attempt to walk for help could find themselves in a deadly situation. The aftermath of a winter storm can have an impact on a community or region for days, weeks, or possibly months. Wind - Some winter storms have extremely strong winds which can create blizzard conditions with blinding, wind driven snow, drifting, and dangerous wind chills. These intense winds can bring down trees and poles, and can also cause damage to homes and other buildings.