Advisory Circular 00-45H Aviation Weather Services
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Chatham Upper Air Site (CHH) Being Decommissioned Effective April 1, 2021 Updated: March 15, 2021
Chatham Upper Air Site (CHH) Being Decommissioned Effective April 1, 2021 Updated: March 15, 2021 The National Weather Service Upper Air Station providing upper air observations from Chatham, Massachusetts - site identifier KCHH, WMO identifier 74494 - will not gather or transmit data after 8 a.m. on March 31. The site will permanently close. Recent significant erosion of the coastal bluff where the upper air station is located is a safety concern for the personnel who launch weather balloons at the facility and threatens to take the upper air launch building into the sea. As a result of these extenuating circumstances, the site will be decommissioned at the end of the month, with demolition of the buildings scheduled for April. The National Weather Service is actively seeking a new site for upper air observations in southeastern New England and will provide the community with updates as we learn more. Nearby upper air sites in Brookhaven, NY (OKX) (latest sounding), Albany, NY (ALY) (latest sounding) and Gray, ME (GYX) (latest sounding) will continue to provide observations for our weather forecast models and help our forecasters deliver accurate and timely watches and warnings. Users of our upper air data can rely on these upper air sites when the Chatham site is decommissioned. Supplemental weather balloon launches at these sites are conducted when weather conditions warrant. These two AWIPS products will cease effective April 1, 2021. They are for the RAOB Mandatory (MAN) and Significant (SGL) levels observations. AWIPS PIL WMO Header MANCHH USUS41 KBOX SGLCHH UMUS41 KBOX National Weather Service upper air stations gather observations using radiosondes. -
Precipitation Effects of Giant Cloud Condensation Nuclei Artificially Introduced Into Stratocumulus Clouds
Atmos. Chem. Phys., 15, 5645–5658, 2015 www.atmos-chem-phys.net/15/5645/2015/ doi:10.5194/acp-15-5645-2015 © Author(s) 2015. CC Attribution 3.0 License. Precipitation effects of giant cloud condensation nuclei artificially introduced into stratocumulus clouds E. Jung1, B. A. Albrecht1, H. H. Jonsson2, Y.-C. Chen3,4, J. H. Seinfeld3, A. Sorooshian5, A. R. Metcalf3,*, S. Song1, M. Fang1, and L. M. Russell6 1Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, FL, USA 2Center for Interdisciplinary Remotely-Piloted Aircraft Studies, Naval Postgraduate School, Monterey, California, USA 3California Institute of Technology, Pasadena, California, USA 4Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA 5Department of Chemical and Environmental Engineering, and Department of Atmospheric Sciences, University of Arizona, Tucson, Arizona, USA 6Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California, USA *now at: Department of Mechanical Engineering, University of Minnesota, Minneapolis, Minnesota, California, USA Correspondence to: E. Jung ([email protected]) Received: 7 November 2014 – Published in Atmos. Chem. Phys. Discuss.: 7 January 2015 Revised: 6 April 2015 – Accepted: 11 April 2015 – Published: 22 May 2015 Abstract. To study the effect of giant cloud condensation 1 Introduction nuclei (GCCN) on precipitation processes in stratocumulus clouds, 1–10 µm diameter salt particles (salt powder) were The stratocumulus (Sc) cloud deck is the most persistent released from an aircraft while flying near the cloud top on cloud type in the world, and the variations of the cloud 3 August 2011 off the central coast of California. The seeded amount and the albedo can significantly impact the climate area was subsequently sampled from the aircraft that was system through their radiative effects on the earth system equipped with aerosol, cloud, and precipitation probes and (e.g., Hartmann et al., 1992; Slingo, 1990). -
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. -
Optimization Requirements Document for the Meteorological Data Collection and Reporting System/ Aircraft Meteorological Data Relay System
Optimization Requirements Document for the Meteorological Data Collection and Reporting System/ Aircraft Meteorological Data Relay System Submitted to: National Oceanic and Atmospheric Administration (NOAA) Order Number DG133W05SE5678 Submitted by: A 2551 Riva Road Annapolis, MD 21401-7465 U.S.A. March 2006 Optimization Requirements Document 1.0 Summary This document presents the requirements and justification for an Optimization System for the Meteorological Data Collection and Reporting System (MDCRS) that will enable selection of specific aircraft to provide essential weather observations to meet the government’s needs while reducing redundant and unnecessary data. MDCRS is a private/public partnership within the U.S. that facilitates the collection of atmospheric measurements from commercial aircraft to improve aviation safety. (MDCRS is similar to the Aircraft Meteorological Data Relay (AMDAR) system that has been implemented in other parts of the world; therefore, the term MDCRS/AMDAR is used in this document to refer to the general program within the U.S. for collecting weather observations from aircraft.) The MDCRS/AMDAR system receives Aircraft Communications Addressing and Reporting System (ACARS) messages containing meteorological data from participating aircraft, processes the messages and forwards the encoded data to NOAA’s National Centers for Environmental Prediction (NCEP), where they are used in weather forecasting models. The system has been in place since 1995 and can arguably be said to provide better and more timely information to weather forecasters than is possible by any other means. High quality meteorological data enable more accurate forecasting of hazardous weather, which directly contributes to the FAA’s goals to increase safety and capacity in the NAS and benefits the airlines directly. -
Overview of Climate Prediction Center
Overview of Climate Prediction Center Dr. Wayne Higgins, Director Climate Prediction Center / NCEP January 26, 2010 Outline • NCEP within National Weather Service • CPC within NCEP • Ongoing CPC Activities • Climate Prediction Advances • Future Opportunities NCEP within NWS National Centers for Environmental Prediction (NCEP) Organization: Central component of NOAA National Weather Service Mission: NCEP delivers science-based environmental predictions to the nation and the global community. We collaborate with partners and customers to produce reliable, timely, and accurate analyses, guidance, forecasts and warnings for the protection of life and property and the enhancement of the national economy. Aviation Weather Center Space Weather Prediction Center NCEP Central Operations Climate Prediction Center Environmental Modeling Center Storm Prediction Center Hydromet Prediction Center Ocean Prediction Center Tropical Prediction Center Vision: The Nation’s trusted source, first alert and preferred partner for environmental prediction services What Does NCEP Do? “From the Sun to the Sea” • Solar Monitoring, Warnings and Forecasts • Climate Forecasts: Weekly to Seasonal to Interannual • El Nino – La Nina Forecast • Weather Forecasts to Day 7 • Hurricanes, Severe Weather, Snowstorms, Fire Weather • Aviation Forecasts and Warnings • Offshore and High Seas Forecasts and Warnings • Model Development, Implementation and Applications for Global and Regional Weather, Climate, Oceans and now Space Weather • International Partnerships in Ensemble Forecasts -
Wind Resource Mapping for United States Offshore Areas (Poster)
WINDWIND RESOURCERESOURCE MAPPINGMAPPING FORFOR UNITEDUNITED STATESSTATES OFFSHOREOFFSHORE AREASAREAS Dennis Elliott and Marc Schwartz National Renewable Energy Laboratory • Golden, Colorado Offshore Wind Mapping Project Offshore Wind Mapping Regions Methodology for Estimating Offshore • Objective is to develop high-resolution validated wind resource maps for Wind Potential priority regions up to 50 nautical miles offshore • Build GIS database elements – East coast areas from Maine to northern Florida – 50 m wind power class – Western Gulf of Mexico (Texas and Louisiana) – Water depth – Great Lakes – Distance from shore – Offshore administrative units • Project is jointly funded by DOE/NREL, states, and other organizations •Datasets created by Mineral Management Service – Wind resource modeling performed by AWS Truewind using MesoMap • Wind resource grid cells (numerical model) system – 200 m x 200 m size – Validation of model data conducted by NREL and collaborators using – Classified by GIS elements available measurement data and other information • Final Products • Offshore wind potential estimates will be made by state and other criteria – Tables of wind resource by state – Documentation and publication of materials Major Data Sets for Offshore Wind Georgia Preliminary 90 m Offshore Wind Speed Georgia Offshore Wind Mapping Assessment and Validation of • Georgia is the first offshore region to be mapped Model Results • Jointly funded by Georgia Environmental Facilities Authority and DOE/NREL • Meteorological station data from National -
Nevada's Weather and Climate
Fact Sheet-17-04 Nevada’s Weather and Climate Kerri Jean Ormerod, Assistant Professor/Extension Program Leader Stephanie McAfee, Assistant Professor/Deputy State Climatologist Introduction different seasons. Every place has its own normal Weather and climate are related, but they are climate. For example, Las Vegas typically gets not the same. The difference between weather thunderstorms in the summer. Much of Nevada and climate is time. Practically speaking, weather gets winter rain or snow when large storms that determines which clothes you decide to put on form over the Pacific head eastward. today, but climate determines the type of clothes Weather and climate are influenced and defined that are in your closet. by a number of factors, including atmospheric pressure, winds, ocean currents, temperature and Weather and Climate Basics topography. Atmospheric pressure (the weight Weather describes the variation of the atmo- of the atmosphere, also known as barometric sphere in a particular place over a short period of pressure) is an important driver of weather and time. Weather conditions include changes in air climate. Weather maps indicate areas of similar pressure, temperature, humidity, clouds, wind and atmospheric pressure with lines called isobars precipitation – rain, hail and snow. Weather can (see Figure 1). Areas with high pressure are change over the course of minutes, hours, days marked H and are typically associated with sun- or weeks. Climate is the usual or expected weather for a particular place or region, which is typically evalu- ated over a 30-year time period referred to as a normal. The timescale for climate is months, sea- sons, years, decades, centuries and even mil- lenia. -
Aviation Weather Services (AC 00-45H)
U.S. Department Advisory of Transportation Federal Aviation Administration Circular Subject: Aviation Weather Services Date: 1/8/18 AC No: 00-45H Initiated by: AFS-400 Change: 1 1 PURPOSE OF THIS ADVISORY CIRCULAR (AC). This AC explains U.S. aviation weather products and services. It provides details when necessary for interpretation and to aid usage. This publication supplements its companion manual, AC 00-6, Aviation Weather, which documents weather theory and its application to aviation. The objective of this AC is to bring the pilot and operator up-to-date on new and evolving weather information and capabilities to help plan a safe and efficient flight, while also describing the traditional weather products that remain. 2 PRINCIPAL CHANGES. This change adds guidance and information on Graphical Forecast for Aviation (GFA), Localized Aviation Model Output Statistics (MOS) Program (LAMP), Terminal Convective Forecast (TCF), Polar Orbiting Environment Satellites (POES), Low-Level Wind Shear Alerting System (LLWAS), and Flight Path Tool graphics. It also updates guidance and information on Direct User Access Terminal Service (DUATS II), Telephone Information Briefing Service (TIBS), and Terminal Doppler Weather Radar (TDWR). This change removes information regarding Area Forecasts (FA) for the Continental United States (CONUS). 1/8/18 AC 00-45H CHG 1 PAGE CONTROL CHART Remove Pages Dated Insert Pages Dated Pages iii thru xii 11/14/16 Pages iii thru xiii 1/8/18 Pages 1-8 and 1-9 11/14/16 Page 1-8 1/8/18 Page 3-57 11/14/16 Pages 3-57 thru -
Chapter 4: Fog
CHAPTER 4: FOG Fog is a double threat to boaters. It not only reduces visibility but also distorts sound, making collisions with obstacles – including other boats – a serious hazard. 1. Introduction Fog is a low-lying cloud that forms at or near the surface of the Earth. It is made up of tiny water droplets or ice crystals suspended in the air and usually gets its moisture from a nearby body of water or the wet ground. Fog is distinguished from mist or haze only by its density. In marine forecasts, the term “fog” is used when visibility is less than one nautical mile – or approximately two kilometres. If visibility is greater than that, but is still reduced, it is considered mist or haze. It is important to note that foggy conditions are reported on land only if visibility is less than half a nautical mile (about one kilometre). So boaters may encounter fog near coastal areas even if it is not mentioned in land-based forecasts – or particularly heavy fog, if it is. Fog Caused Worst Maritime Disaster in Canadian History The worst maritime accident in Canadian history took place in dense fog in the early hours of the morning on May 29, 1914, when the Norwegian coal ship Storstadt collided with the Canadian Pacific ocean liner Empress of Ireland. More than 1,000 people died after the Liverpool-bound liner was struck in the side and sank less than 15 minutes later in the frigid waters of the St. Lawrence River near Rimouski, Quebec. The Captain of the Empress told an inquest that he had brought his ship to a halt and was waiting for the weather to clear when, to his horror, a ship emerged from the fog, bearing directly upon him from less than a ship’s length away. -
Innovative Mini Ultralight Radioprobes to Track Lagrangian Turbulence Fluctuations Within Warm Clouds: Electronic Design
sensors Article Innovative Mini Ultralight Radioprobes to Track Lagrangian Turbulence Fluctuations within Warm Clouds: Electronic Design Miryam E. Paredes Quintanilla 1,* , Shahbozbek Abdunabiev 1, Marco Allegretti 1, Andrea Merlone 2 , Chiara Musacchio 2 , Eros G. A. Pasero 1, Daniela Tordella 3 and Flavio Canavero 1 1 Politecnico di Torino, Department of Electronics and Telecommunications (DET), Corso Duca Degli Abruzzi 24, 10129 Torino, Italy; [email protected] (S.A.); [email protected] (M.A.); [email protected] (E.G.A.P.); fl[email protected] (F.C.) 2 Istituto Nazionale di Ricerca Metrologica, Str. Delle Cacce, 91, 10135 Torino, Italy; [email protected] (A.M.); [email protected] (C.M.) 3 Politecnico di Torino, Department of Applied Science and Technology (DISAT), Corso Duca Degli Abruzzi 24, 10129 Torino, Italy; [email protected] * Correspondence: [email protected] Abstract: Characterization of dynamics inside clouds remains a challenging task for weather forecast- ing and climate modeling as cloud properties depend on interdependent natural processes at micro- and macro-scales. Turbulence plays an important role in particle dynamics inside clouds; however, turbulence mechanisms are not yet fully understood partly due to the difficulty of measuring clouds at the smallest scales. To address these knowledge gaps, an experimental method for measuring the influence of small-scale turbulence in cloud formation in situ and producing an in-field cloud Citation: Paredes Quintanilla, M.E.; Lagrangian dataset is being developed by means of innovative ultralight radioprobes. This paper Abdunabiev, S.; Allegretti, M.; presents the electronic system design along with the obtained results from laboratory and field exper- Merlone, A.; Musacchio, C.; Pasero, ≈ ≈ E.G.A.; Tordella, D.; Canavero, F. -
On the Use of Radiosondes in Freezing Precipitation
MARCH 2018 W AUGH AND SCHUUR 459 On the Use of Radiosondes in Freezing Precipitation SEAN WAUGH NOAA/OAR/National Severe Storms Laboratory, and Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma, Norman, Oklahoma TERRY J. SCHUUR Cooperative Institute for Mesoscale Meteorological Studies, University of Oklahoma, and NOAA/OAR/National Severe Storms Laboratory, Norman, Oklahoma (Manuscript received 13 April 2017, in final form 4 January 2018) ABSTRACT Radiosonde observations are used the world over to provide critical upper-air observations of the lower atmosphere. These observations are susceptible to errors that must be mitigated or avoided when identified. One source of error not previously addressed is radiosonde icing in winter storms, which can affect forecasts, warning operations, and model initialization. Under certain conditions, ice can form on the radiosonde, leading to decreased response times and incorrect readings. Evidence of radiosonde icing is presented for a winter storm event in Norman, Oklahoma, on 24 November 2013. A special sounding that included a particle imager probe and a GoPro camera was flown into the system producing ice pellets. While the iced-over temperature sensor showed no evidence of an elevated melting layer (ML), complementary Particle Size, Image, and Velocity (PASIV) probe and polarimetric radar observations provide clear evidence that an ML was indeed present. Radiosonde icing can occur while passing through a layer of supercooled drops, such as frequently found in a subfreezing layer that often lies below the ML in winter storms. Events that have warmer/deeper MLs would likely melt any ice present off the radiosonde, minimizing radiosonde icing and allowing the ML to be detected. -
Aviation Hazards (In 3 Parts) Talking Points, Notes and Extras (Extensive List of Links)
Aviation Hazards (in 3 Parts) Talking Points, Notes and Extras (Extensive List of Links) Part 1 – Aviation Hazards: Page 1 Title/Welcome/Intro Page. Artwork: “Airborne Trailblazer” by Ms. Lane E. Wallace Page 2 Overall Objectives of the Aviation Hazards development plan – all three parts. Page 3 The six(plus) categories that will be covered in the entire module. Page 4 The specific objectives of Part 1. Page 5 William Henry Dines…famous meteorologist of the late 19th through early 20th century. Developed the Pressure Tube (Dines) Anemometer. Did much of his best and most renown work on upper air meteorology – involving kites, (later) balloons and meteorographs (starting in 1901). His meteorographs where famous for being small, lightweight (2oz.) and economical. Member of the Royal Meteorological Society from 1881 until his death in 1928 (president from 1901 through 1902). The “difficulties” he refers to are with regard to both pilot and (forecast) meteorologist – and were: Wind, fog, and clouds. These and other “difficulties” will be addressed throughout the rest of this session. Page 6 (Plus 3) Aviation Weather Center (AWC) – A NOAA/NWS National Support Center that disseminates consistent, timely and accurate weather information for the world airspace system. Disseminates In-flight advisories (AIRMETs, SIGMETs) and provides a portal to much aviation data, such as Aviation Digital Data Service(ADDS). An AIRMET (AIRman's METeorological Information) advises of weather potentially hazardous to all aircraft but that does not meet SIGMET criteria. SIGMETS (Significant Meteorological Information) are issued and amended to warn pilots of weather conditions that are potentially hazardous to all size aircraft and all pilots, such as severe icing or severe turbulence.