1) on a Certain Day, the Isobars on a Weather Map Are Very Close
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Chapter 7.0 – Determining Wind Direction Section 7.1 Overview Of
Chapter 7.0 – Determining Wind Direction Section 7.1 Overview of Wind Direction The wind direction is a measure or indication of where the air movement originated from. The wind direction can be measured through the use of a wind sock, wind vane, or a light object attached to a pole and string (example: A ping pong ball attached to a string which is tied to a stick). Wind direction is generally reported in either Azimuth degrees or Cardinal direction. Azimuth uses a circle with the northern most position indicating 0 degrees. The Cardinal direction system gives an Azimuth degree value a name. For example, 180 degrees is South(S) and 270 degrees is West (W) (See Figure 18 - A basic compass rose). Figure 18 - A basic compass rose Section 7.2 Overview of the homemade Wind Vane The wind vane used in this design was a homemade wind vane using a miniature absolute magnetic shaft encoder. The encoder chosen for use was the MA3 produced by US Digital. The purpose for choosing this specific encoder in regards to this design was that the MA3 met four (4) critical objectives. First, the MA3 was the correct size for the application. Second, the MA3 uses an analog output of 0 volts to 5 volts with respect to the current positions (See Figure 19 – MA3 Output behaviour) Figure 19 – MA3 Output behaviour Third, the MA3 uses a 5 volt input. This was a major consideration when choosing an encoder as a 5 volt input allowed for a more simple integration. Fourth, and final, the MA3 met the requirements of being able to function in an adverse environment, having an operational temperature of -40 ºC to +125 ºC. -
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. -
The Hemlock Woolly Adelgid in Georgia
ASSESSMENT OF SASAJISCYMNUS TSUGAE, SCYMNUS SINUANODULUS, AND LARICOBIUS NIGRINUS: PREDATOR BEETLES RELEASED TO CONTROL THE HEMLOCK WOOLLY ADELGID IN GEORGIA by CERA ELIZABETH JONES (Under the Direction of James L. Hanula) ABSTRACT Eastern hemlock, Tsuga canadensis, and Carolina hemlock, Tsuga caroliniana, are being threatened by the invasive hemlock woolly adelgid, Adelges tsugae. Adelges tsugae, is currently found throughout most of the range of T. canadensis and the entire range of T. caroliniana and arrived in Georgia in 2003. In an attempt to preserve the hemlocks, biological control predatory beetles Sasajiscymnus tsugae, Laricobius nigrinus, and Scymnus sinuanodulus are being mass reared and released. The objectives considered in this research are to: 1. Determine establishment of these biological control agents in the North Georgia mountains. 2. To determine aestivation survival and time of emergence of L. nigrinus. INDEX WORDS: Adelges tsugae, Sasajiscymnus tsugae, Laricobius nigrinus, Scymnus sinuanodulus, Tsuga canadensis, Tsuga caroliniana, biological control, emergence, recovery, establishment, aestivation ASSESSING THE ESTABLISHMENT OF SASAJISCYMNUS TSUGAE, SCYMNUS SINUANODULUS, AND LARICOBIUS NIGRINUS: PREDATOR BEETLES RELEASED TO CONTROL THE HEMLOCK WOOLLY ADELGID IN GEORGIA by CERA ELIZABETH JONES B.S., Baldwin-Wallace College, 2006 A Thesis Submitted to the Graduate Faculty of The University of Georgia in Partial Fulfillment of the Requirements for the Degree MASTER OF SCIENCE ATHENS, GEORGIA 2013 © 2013 Cera Elizabeth Jones All Rights Reserved ASSESSING THE ESTABLISHMENT OF SASAJISCYMNUS TSUGAE, SCYMNUS SINUANODULUS, AND LARICOBIUS NIGRINUS: PREDATOR BEETLES RELEASED TO CONTROL THE HEMLOCK WOOLLY ADELGID IN GEORGIA by CERA ELIZABETH JONES Major Professor: James L. Hanula Committee: S. Kristine Braman Kamal Gandhi Electronic Version Approved Maureen Grasso Dean of Graduate School The University of Georgia December 2013 ACKNOWLEDGEMENTS I would like to especially thank my advisor Dr. -
Impact of Cloud Analysis on Numerical Weather Prediction in the Galician Region of Spain
Impact of Cloud Analysis on Numerical Weather Prediction in the Galician Region of Spain M. J. SOUTO, C. F. BALSEIRO AND V. P…REZ-MU—UZURI Group of Nonlinear Physics, Faculty of Physics, University of Santiago de Compostela, Santiago de Compostela, Spain Ming Xue University of Oklahoma, School of Meteorology, and CAPS Oklahoma, USA Keith BREWSTER Center for Analysis and Prediction of Storms, Oklahoma, USA April, 2001 Revised December, 2001 Corresponding author address: Dra. M. J. Souto, Group of Nonlinear Physics Faculty of Physics, University of Santiago de Compostela E-15706, Santiago de Compostela, Spain e-mail: [email protected] ABSTRACT The Advanced Regional Prediction System (ARPS) is applied to operational numerical weather forecast in Galicia, northwest Spain. A 72-hour forecast at a 10-km horizontal resolution is produced dta for the region. Located on the northwest coast of Spain and influenced by the Atlantic weather systems, Galicia has a high percentage (almost 50%) of rainy days per year. For these reasons, the precipitation processes and the initialization of moisture and cloud fields are very important. Even though the ARPS model has a sophisticated data analysis system (ADAS) that includes a 3D cloud analysis package, due to operational constraint, our current forecast starts from 12-hour forecast of the NCEP AVN model. Still, procedures from the ADAS cloud analysis are being used to construct the cloud fields based on AVN data, and then applied to initialize the microphysical variables in ARPS. Comparisons of the ARPS predictions with local observations show that ARPS can predict quite well both the daily total precipitation and its spatial distribution. -
Global Warming Climate Records
ATM S 111: Global Warming Climate Records Jennifer Fletcher Day 24: July 26 2010 Reading For today: “Keeping Track” (Climate Records) pp. 171-192 For tomorrow/Wednesday: “The Long View” (Paleoclimate) pp. 193-226. The Instrumental Record from NASA Global temperature since 1880 Ten warmest years: 2001-2009 and 1998 (biggest El Niño ever) Separation into Northern/ Southern Hemispheres N. Hem. has warmed more (1o C vs 0.8o C globally) S. Hem. has warmed more steadily though Cooling in the record from 1940-1975 essentially only in the N. Hem. record (this is likely due to aerosol cooling) Temperature estimates from other groups CRUTEM3 (RG calls this UEA) NCDC (RG calls this NOAA) GISS (RG calls this NASA) yet another group Surface air temperature over land Thermometer between 1.25-2 m (4-6.5 ft) above ground White colored to reflect away direct sunlight Slats to ensure fresh air circulation “Stevenson screen”: invented by Robert Louis Stevenson’s dad Thomas Yearly average Central England temperature record (since 1659) Temperatures over Land Only NASA separates their analysis into land station data only (not including ship measurements) Warming in the station data record is larger than in the full record (1.1o C as opposed to 0.8o C) Sea surface temperature measurements Standard bucket Canvas bucket Insulated bucket (~1891) (pre WWII) (now) “Bucket” temperature: older style subject to evaporative cooling Starting around WWII: many temperature measurements taken from condenser intake pipe instead of from buckets. Typically 0.5 C warmer -
Atmospheric Thermal and Dynamic Vertical Structures of Summer Hourly Precipitation in Jiulong of the Tibetan Plateau
atmosphere Article Atmospheric Thermal and Dynamic Vertical Structures of Summer Hourly Precipitation in Jiulong of the Tibetan Plateau Yonglan Tang 1, Guirong Xu 1,*, Rong Wan 1, Xiaofang Wang 1, Junchao Wang 1 and Ping Li 2 1 Hubei Key Laboratory for Heavy Rain Monitoring and Warning Research, Institute of Heavy Rain, China Meteorological Administration, Wuhan 430205, China; [email protected] (Y.T.); [email protected] (R.W.); [email protected] (X.W.); [email protected] (J.W.) 2 Heavy Rain and Drought-Flood Disasters in Plateau and Basin Key Laboratory of Sichuan Province, Institute of Plateau Meteorology, China Meteorological Administration, Chengdu 610072, China; [email protected] * Correspondence: [email protected]; Tel.: +86-27-8180-4913 Abstract: It is an important to study atmospheric thermal and dynamic vertical structures over the Tibetan Plateau (TP) and their impact on precipitation by using long-term observation at represen- tative stations. This study exhibits the observational facts of summer precipitation variation on subdiurnal scale and its atmospheric thermal and dynamic vertical structures over the TP with hourly precipitation and intensive soundings in Jiulong during 2013–2020. It is found that precipitation amount and frequency are low in the daytime and high in the nighttime, and hourly precipitation greater than 1 mm mostly occurs at nighttime. Weak precipitation during the daytime may be caused by air advection, and strong precipitation at nighttime may be closely related with air convection. Both humidity and wind speed profiles show obvious fluctuation when precipitation occurs, and the greater the precipitation intensity, the larger the fluctuation. Moreover, the fluctuation of wind speed Citation: Tang, Y.; Xu, G.; Wan, R.; Wang, X.; Wang, J.; Li, P. -
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. -
Comparative Cold Tolerance and Climate Matching Of
Biological Control 58 (2011) 96–102 Contents lists available at ScienceDirect Biological Control journal homepage: www.elsevier.com/locate/ybcon Comparative cold tolerance and climate matching of coastal and inland Laricobius nigrinus (Coleoptera: Derodontidae), a biological control agent of hemlock woolly adelgid ⇑ D.L. Mausel , R.G. Van Driesche, J.S. Elkinton University of Massachusetts, Department of Plant, Soil and Insect Science, 102 Fernald Hall, Amherst, MA 01003, United States article info abstract Article history: Laricobius nigrinus (Coleoptera: Derodontidae) was first collected near the coastal city of Victoria, British Received 1 June 2010 Columbia, Canada for release as a biological control agent to suppress tree-killing densities of hemlock Accepted 8 April 2011 woolly adelgid, Adelges tsugae (Hemiptera: Adelgidae), in the eastern United States. Beetles established Available online 20 April 2011 in warm areas of the invaded range of A. tsugae, but had a low probability of establishment in cold areas. With the goal of locating beetles with greater cold-tolerance, we collected hundreds of adults in the Keywords: northern Rocky Mountains. To support planned releases of these inland L. nigrinus, the cold tolerance Tsuga canadensis of field-collected coastal (Seattle, WA) and inland (Coeur d’Alene and Moscow, ID) adults and climate Adelges tsugae match index scores (CLIMEX v.2) of these collection areas and parts of the eastern United States were Laricobius nigrinus Classical biological control compared. We found that individuals of inland L. nigrinus were more cold tolerant than those of coastal Intraspecific variation L. nigrinus, based on higher survival in a winter field cage study in Massachusetts and a lower superco- Cold tolerance oling point in a laboratory assay. -
The Measurement of Tropospheric
EPJ Web of Conferences 119,27004 (2016) DOI: 10.1051/epjconf/201611927004 ILRC 27 THE MEASUREMENT OF TROPOSPHERIC TEMPERATURE PROFILES USING RAYLEIGH-BRILLOUIN SCATTERING: RESULTS FROM LABORATORY AND ATMOSPHERIC STUDIES Benjamin Witschas1*, Oliver Reitebuch1, Christian Lemmerz1, Pau Gomez Kableka1, Sergey Kondratyev2, Ziyu Gu3, Wim Ubachs3 1German Aerospace Center (DLR), Institute of Atmospheric Physics, 82234 Oberpfaffenhofen, Germany 2Angstrom Ltd., 630090 Inzhenernaya16, Novosibirsk, Russia 3Department of Physics and Astronomy, LaserLaB, VU University, 1081 HV Amsterdam, Netherlands *Email: [email protected] ABSTRACT are only applicable to stratospheric or meso- In this letter, we suggest a new method for spheric measurements because they can only be measuring tropospheric temperature profiles using applied in air masses that do not contain aerosols, Rayleigh-Brillouin (RB) scattering. We report on or where appropriate fluorescing metal atoms laboratory RB scattering measurements in air, exist. In contrast, Raman lidars can be applied for demonstrating that temperature can be retrieved tropospheric measurements [2]. Nevertheless, it from RB spectra with an absolute accuracy of has to be mentioned that the Raman scattering better than 2 K. In addition, we show temperature cross section is quite low. Thus, powerful lasers, profiles from 2 km to 15.3 km derived from RB sophisticated background filters, or night-time spectra, measured with a high spectral resolution operation are required to obtain reliable results. In lidar during daytime. A comparison with particular, the rotational Raman differential radiosonde temperature measurements shows backscattering cross section (considering Stokes reasonable agreement. In cloud-free conditions, and anti-Stokes branches) is about a factor of 50 the temperature difference reaches up to 5 K smaller than the one of Rayleigh scattering [3]. -
An Objective Determination of Probability of Fog Formation *
158 BULLETIN AMERICAN METEOROLOGICAL SOCIETY An Objective Determination of Probability of Fog Formation * LOUIS BERKOFSKY Atmospheric Analysis Laboratory, Base Directorate for Geophysical Research, Air Force Cambridge Research Laboratories, 230 Albany St., Cambridge, Mass. ABSTRACT A method of approach to objective fog forecasting, based on the use of probability charts is suggested. Given two parameters, say wind speed and dew-point depression, at sunset as ordinate and abscissa of a chart, occurrences and non-occurrences of fog following sunset are plotted as functions of these parameters. Isolines of relative frequency are drawn, giving a probability chart. Two more such charts, using four additional parameters, are constructed, and a total probability of fog occurrence following sunset is computed as a linear function of the three individual probabilities. This result is used as a criterion for the forecast. Time of formation equations are developed, to be applied in the event a fog proves to be likely. I. INTRODUCTION sive—during which period the fog was mainly non-frontal. Only those cases were considered in ANY objective methods of forecasting which precipitation was not occurring at time of fog deal primarily with determination of fog formation, in order to simplify the investiga- time of formation. The determination M tion.1 of likelihood of formation is largely subjective. If it is decided subjectively that a fog must be II. THE PARAMETERS forecast, the objective time graphs are then en- No so-called objective method is truly objective, tered. Such graphs must of necessity consider due to the fact that it is necessary for the investi- only cases of occurrence, and therefore should gator to select certain parameters. -
The Role of Wind in Rainwater Catchment and Fog Collection by Robert S
Water International (1994) Vol 19, pp 70-76 The Role of Wind in Rainwater Catchment and Fog Collection by Robert S. Schemenauer, M. IWRA Environment Canada 4905 Dufferin Street DOWNSVIEW ON M3H 5T4 CANADA and Pilar Cereceda Institute of Geography Pontifical Catholic University of Chile Casilia 306, Correo 22 SANTIAGO CHILE ABSTRACT Water droplets in the atmosphere typically range in size from the smallest cloud or fog droplets, with diameters of lmm, to the largest raindrops with diameters of about 5 mm. The fog droplets have negligible fall velocities and their trajectories are determined by the speed and direction of the wind. Raindrops have fall velocities (2 to 9 m/s) comparable to typical wind speeds and, therefore, will fall at an angle, except in unusual circumstances where the wind speed is zero. An understanding of the fall angle of rain and drizzle drops can lead to a better orientation and design of rooftop rainwater catchment systems and, in certain environments, to the collection of substantially more water. This leads to five recommendations: first, that as the wind speed increases or the drop sizes decrease, the vertical component of rainwater catchment systems should be enhanced; second, wind direction, wind speed, and rainfall rate information should be used to optimize the orientation of the house and the shape and slope of the root third, that use should be made of upwind walls of houses as rain collectors,' fourth, that in foggy environments rainwater catchment systems be modified to collect fog water as well,' and fifth, that tree plantations in arid regions should be designed in a manner that optimizes their role as fog collectors. -
A Simple Lumped Model to Convert Air Temperature Into Surface Water
EGU Journal Logos (RGB) Open Access Open Access Open Access Advances in Annales Nonlinear Processes Geosciences Geophysicae in Geophysics Open Access Open Access Natural Hazards Natural Hazards and Earth System and Earth System Sciences Sciences Discussions Open Access Open Access Atmospheric Atmospheric Chemistry Chemistry and Physics and Physics Discussions Open Access Open Access Atmospheric Atmospheric Measurement Measurement Techniques Techniques Discussions Open Access Open Access Biogeosciences Biogeosciences Discussions Open Access Open Access Climate Climate of the Past of the Past Discussions Open Access Open Access Earth System Earth System Dynamics Dynamics Discussions Open Access Geoscientific Geoscientific Open Access Instrumentation Instrumentation Methods and Methods and Data Systems Data Systems Discussions Open Access Open Access Geoscientific Geoscientific Model Development Model Development Discussions Open Access Open Access Hydrol. Earth Syst. Sci., 17, 3323–3338, 2013 Hydrology and Hydrology and www.hydrol-earth-syst-sci.net/17/3323/2013/ doi:10.5194/hess-17-3323-2013 Earth System Earth System © Author(s) 2013. CC Attribution 3.0 License. Sciences Sciences Discussions Open Access Open Access Ocean Science Ocean Science Discussions A simple lumped model to convert air temperature into surface Open Access Open Access water temperature in lakes Solid Earth Solid Earth Discussions S. Piccolroaz, M. Toffolon, and B. Majone Department of Civil, Environmental and Mechanical Engineering, University of Trento, Italy Open Access Open Access Correspondence to: S. Piccolroaz ([email protected]) The Cryosphere Received: 23 January 2013 – Published in Hydrol. Earth Syst. Sci. Discuss.: 5 March 2013The Cryosphere Discussions Revised: 4 July 2013 – Accepted: 20 July 2013 – Published: 27 August 2013 Abstract. Water temperature in lakes is governed by a com- show remarkable agreement with measurements over the en- plex heat budget, where the estimation of the single fluxes tire data period.