JO 7900.5E, Surface Weather Observing

Total Page:16

File Type:pdf, Size:1020Kb

JO 7900.5E, Surface Weather Observing U.S. DEPARTMENT OF TRANSPORTATION ORDER FEDERAL AVIATION ADMINISTRATION JO 7900.5E Air Traffic Organization Policy Effective Date: 01/15/2020 SUBJ: Surface Weather Observing The Federal Aviation Administration (FAA) Surface Weather Observer Program is a component of the National Airspace System (NAS). It combines with other elements of the NAS to ensure the overall safety of air transportation services. The FAA is committed to providing the resources necessary to ensure the vibrancy of this critical aviation service. This order provides the practices and procedures for weather observation services that support the important role it plays in the mission of the FAA. The practices and procedures set forth in this order apply to all FAA personnel, FAA-contract personnel, and non-Federal Observer personnel who provide aviation weather observation services. Weather observer personnel are required to apply the provision of this order as it pertains to their observational responsibilities. Observers are expected to exercise experienced judgment when encountering situations not covered by this order. Jeffrey U. Vincent Vice President Air Traffic Services Distribution: Electronic Initiated By: AJT-2 01/15/2020 JO 7900.5E Table of Contents Chapter 1. Introduction ................................................................................................. 1 1.1. Purpose of This Order ..................................................................................................... 1 1.2. Audience. ........................................................................................................................ 1 1.3. Where to Find This Order ............................................................................................... 1 1.4. Cancellation .................................................................................................................... 1 1.5. Explanation of Changes .................................................................................................. 1 1.6. Abbreviations and Acronyms ......................................................................................... 2 1.7. Relationship to FMH-1 and Other Documents ............................................................... 2 1.8. Applicability of Procedures and Practices ...................................................................... 3 1.9. User Responsibilities ...................................................................................................... 3 1.10. Distribution ..................................................................................................................... 4 1.11. Changing the Order ......................................................................................................... 4 1.12. Maintaining the Order ..................................................................................................... 4 Chapter 2. Guidelines ................................................................................................... 5 2.1. Introduction. .................................................................................................................... 5 2.2. Types of Stations ............................................................................................................. 5 2.3. Non-Federal Weather Observation (NF-OBS) Station ................................................... 5 2.4. General Types of Observations ....................................................................................... 5 2.5. Augmentation Requirements .......................................................................................... 6 2.6. Backup Requirements ..................................................................................................... 7 2.7. Evaluating Weather Sensor Accuracy ............................................................................. 8 Chapter 3. General Procedures .................................................................................. 10 3.1. Introduction ................................................................................................................... 10 3.2. Certification of Personnel and Currency Requirements................................................ 10 3.3. Definitions ..................................................................................................................... 10 3.4. Aviation Weather Observing Locations ........................................................................ 12 3.5. General Observing Practices ......................................................................................... 12 3.6. Dissemination ............................................................................................................... 13 3.7. Corrections to Transmitted Data ................................................................................... 14 3.8. Delayed Reports (Manual Stations Only) ..................................................................... 14 3.9. Rounding Off Numbers ................................................................................................. 15 3.10. Record Keeping and Forms .......................................................................................... 15 3.11. Criteria for SPECI Observations ................................................................................... 15 3.12. Content of METAR/SPECI Observations ..................................................................... 17 Chapter 4. General Procedures at Automated Weather Stations ................................ 28 4.1. Purpose .......................................................................................................................... 28 4.2. Types of Automated Stations ........................................................................................ 28 4.3. Procedures for Handling Aircraft Mishaps at Automated Sites .................................... 29 Chapter 5. Augmentation Requirements at Automated Weather Stations .................. 30 5.1. Introduction. .................................................................................................................. 30 5.2. Validity of Data ............................................................................................................. 30 5.3. Sign On/Sign Off the Automated Weather Observing Systems ................................... 30 ii 01/15/2020 JO 7900.5E 5.4. Augmentation Observing Procedures ........................................................................... 31 5.5. General Reporting Procedures ...................................................................................... 32 Chapter 6. Backup/Editing Requirements at Automated Weather Stations ................. 35 6.1. Introduction. .................................................................................................................. 35 6.2. Validity of Data ............................................................................................................. 35 6.3. Equipment Requirements .............................................................................................. 35 6.4. Procedures for Providing Backup Information. ............................................................ 37 6.5. Coding of Missing Data ................................................................................................ 38 6.6. Procedures for Wind Speed and Wind Direction .......................................................... 38 6.7. Procedures for Visibility ............................................................................................... 38 6.8. Procedures for Present Weather and Obscurations ....................................................... 39 6.9. Procedures for Sky Condition. ...................................................................................... 40 6.10. Procedures for Temperature and Dew Point (See Chapter 11) .................................... 40 6.11. Procedures for Altimeter Setting (See Chapter 12) ..................................................... 41 6.12. Malfunctions/Outages ................................................................................................... 42 Chapter 7. Wind .......................................................................................................... 43 7.1. Introduction. .................................................................................................................. 43 7.2. Definitions ..................................................................................................................... 43 7.3. Observing, Determining, and Reporting Procedures .................................................... 43 7.4. Wind Direction. ............................................................................................................. 43 7.5. Estimating Wind Direction ........................................................................................... 44 7.6. Variable Wind Direction ............................................................................................... 44 7.7. Wind Shifts ................................................................................................................... 44 7.8. Wind Speed. .................................................................................................................. 45 7.9. Estimating Wind Speed. ................................................................................................ 45 7.10. Wind
Recommended publications
  • Geometric Characteristics of Clouds from Ceilometer Measurements and Radiosounding Methods
    GEOMETRIC CHARACTERISTICS OF CLOUDS FROM CEILOMETER MEASUREMENTS AND RADIOSOUNDING METHODS Montserrat Costa Surós Dipòsit legal: Gi. 1888-2014 http://hdl.handle.net/10803/284084 http://creativecommons.org/licenses/by/4.0/deed.ca Aquesta obra està subjecta a una llicència Creative Commons Reconeixement Esta obra está bajo una licencia Creative Commons Reconocimiento This work is licensed under a Creative Commons Attribution licence GEOMETRIC CHARACTERISTICS OF CLOUDS FROM CEILOMETER MEASUREMENTS AND RADIOSOUNDING METHODS DOCTORAL THESIS Montserrat Costa Surós 2014 DOCTORAL THESIS GEOMETRIC CHARACTERISTICS OF CLOUDS FROM CEILOMETER MEASUREMENTS AND RADIOSOUNDING METHODS Montserrat Costa Surós 2014 Doctoral Programme in Experimental Sciences and Sustainability Supervisors: Josep Calbó Angrill José Abel González Gutiérrez Thesis submitted for the degree of Doctor of Philosophy by the University of Girona El Dr. Josep Calbó Angrill i el Dr. José Abel González Gutiérrez, professors titulars del Departament de Física de la Universitat de Girona, CERTIFIQUEN: Que aquest treball, titulat “Geometric characteristics of clouds from ceilometer measurements and radiosounding methods”, que presenta la Montserrat Costa Surós per a l’obtenció del títol de doctora, ha estat realitzat sota la seva direcció. I, perquè així consti i tingui els efectes oportuns, signen aquest document. Dr. Josep Calbó Angrill Dr. José Abel González Gutiérrez Girona, 29 de juliol de 2014. Un esforç total és una victòria completa M. Ghandi Acknowledgments First and the most important I would like to thank my supervisors Dr. Josep Calbó and Dr. Josep- Abel González for giving me the opportunity to begin my research career with them, which has led to this doctoral thesis, and for their guidance and support during these years.
    [Show full text]
  • Central Region Technical Attachment 92-11 Using New Technology To
    /Ou)%-c<v^A cU-i CRH SSD MAY 1992 CENTRAL REGION TECHNICAL ATTACHMENT 92-11 USING NEW TECHNOLOGY TO LOCATE AND FORECAST THE MOVEMENT OF A FRONT IN THE MESOSCALE MICHAEL K. HOLZINGER NATIONAL WEATHER SERVICE FORECAST OFFICE DENVER, COLORADO 1. INTRODUCTION The National Weather Service (NWS) is testing much of the future technology in an operational environment at the Weather Service Forecast Office (WSFO) in Denver, Colorado. The Denver AWIPS Risk Reduction and Requirements Evaluation (DARRRE II) workstat­ ion at the WSFO gives forecasters the ability to analyze mesosc- ale features in much more detail and make local forecasts with more precision than was possible a few years ago. WSFO Denver conducted an experimental project, called the En­ hanced Terminal Forecast (EFT) program, between January and November, 1991 (NWS 1990; NWS 1991). In place of standard avia­ tion terminal forecasts, EFT forecasts were issued for the three terminals in the Denver metropolitan area. These are Stapleton International Airport (DEN), Centennial Airport (APA), and Jefferson County Airport (BJC) (Fig. 1A). Compared to conven­ tional terminal forecasts, the EFT had a slightly different format, slightly different amendment criteria, disallowed the use of terms "chance" and "slight chance" during the first three hours, and attempted to nail down weather changes to the nearest 15 minutes during the first three hours. Perhaps, the best opportunity to attempt forecasts to the nearest 15 minutes along the Front Range is provided by warm season wind shifts, either gust fronts or frontal. Warm season wind shifts can often be spotted on Doppler radar an hour or more before they reach DEN.
    [Show full text]
  • Winter Storm Preparedness and Response
    Winter Storm Preparedness and Response SAFETY AT HOME AND WHILE TRAVELING BE AWARE OF THE FORECAST Winter weather advisory. Formerly called a “Travelers’ Advisory,” this Winter storms are worth * serious consideration In alert may be issued by the National Weather Service for a variety of Illinois. Blizzards, heavy severe conditions. Weather advisories may be announced for snow, snow, freezing rain and blowing and drifting snow, freezing drizzle, freezing rain (when less sub-zero temperatures hit hard than ice storm conditions are expected), or a combination of weather and frequently across the events. state. Even if you think you are safe and warm at home, a * Winter storm watch. Severe winter weather conditions may affect your winter storm can become area (freezing rain, sleet or heavy snow may occur either separately or dangerous If the power is cut in combination). off. With a little planning, you can protect yourself and your * Winter storm warning. Severe winter weather conditions are imminent. family from the many hazards of winter weather, both at Freezing rain or freezing drizzle. Rain or drizzle is likely to freeze upon home and on the road. * impact, resulting in a coating of ice glaze on roads and all other exposed objects. * Sleet. Small particles of ice, usually mixed with rain. If enough sleet accumulates on the ground, it makes travel hazardous. * Blizzard warning. Sustained wind speeds of at least 35 miles per hour are accompanied by considerable failing and/or blowing snow. This is the most perilous winter storm, with visibility dangerously restricted. * Wind chill. A strong wind combined with a temperature slightly below freezing can have the same chilling effect as a temperature nearly 50 degrees lower in a calm atmosphere.
    [Show full text]
  • AMOFSG/10-Sod 19/6/13
    AMOFSG/10-SoD 19/6/13 AERODROME METEOROLOGICAL OBSERVATION AND FORECAST STUDY GROUP (AMOFSG) TENTH MEETING Montréal, 17 to 19 June 2013 SUMMARY OF DISCUSSIONS 1. HISTORICAL 1.1 The tenth meeting of the Aerodrome Meteorological Observation and Forecast Study Group (AMOFSG) was held at the Headquarters of the International Civil Aviation Organization (ICAO) in Montréal, Canada, 17 to 19 June 2013. 1.2 The meeting was opened by Mr. Greg Brock, Chief of the Meteorology Section of the Air Navigation Bureau of ICAO, who extended a warm welcome to all the participants. Mr. Brock emphasized that this tenth meeting of the AMOFSG was likely to be the last of the group prior to the convening of an ICAO Meteorology (MET) Divisional Meeting in July 2014, to be held in part conjointly with the Fifteenth Session of the World Meteorological Organization (WMO) Commission for Aeronautical Meteorology (CAeM-XV). For this reason, Mr. Brock underlined the need for the group to work efficiently during its three days of deliberations, with a strong emphasis placed on determining whether proposals arising from each of the topics to be addressed were of sufficient maturity so as to reduce or eliminate entirely the need for significant further work and/or a meeting ahead of the MET Divisional Meeting. 1.3 The names and contact details of the participants are listed in Appendix A . Mr. Bill Maynard was elected Chairman of the meeting. The meeting was served by the Acting Secretary of the AMOFSG, Mr. Greg Brock, Chief, Meteorology Section. 1.4 The meeting considered the following agenda items: Agenda Item 1: Opening of the meeting; Agenda Item 2: Election of Chairman; Agenda Item 3: Adoption of working arrangements; Agenda Item 4: Adoption of the agenda; (41 pages) AMOFSG.10.SoD.en.docx AMOFSG/10-SoD - 2 - Agenda Item 5: Aerodrome observations; Agenda Item 6: Forecasting at the aerodrome and in the terminal area and ATIS requirements; Agenda Item 7: Deliverables; Agenda Item 8: Any other business; and Agenda Item 9: Closure of the meeting.
    [Show full text]
  • Performance Evaluation of Misting Fans in Hot and Humid Climate
    Building and Environment 45 (2010) 2666e2678 Contents lists available at ScienceDirect Building and Environment journal homepage: www.elsevier.com/locate/buildenv Performance evaluation of misting fans in hot and humid climate N.H. Wong*, Adrian Z.M. Chong Department of Building, School of Design and Environment, National University of Singapore, 117566 Republic of Singapore article info abstract Article history: Singapore experiences a hot and humid climate throughout the year. This in turn results in heavy reli- Received 3 March 2010 ance on mechanical systems especially air-conditioning to achieve thermal comfort. An alternative would Received in revised form be the use of evaporative cooling which is less energy intensive. Objective and subjective measurements 14 May 2010 were conducted at an experimental setup at the National University of Singapore (NUS) to evaluate the Accepted 27 May 2010 thermal conditions and thermal sensations brought about by misting fans. Field measurements were also conducted at food centres in Singapore to determine if they are coherent with the objective and Keywords: subjective measurements conducted. Analysis of objective and subjective data showed that the misting Misting fan fi Evaporative cooling fan was able to signi cantly reduce the dry-bulb temperature and thermal sensation votes. This is fi Singapore consistent with eld measurements taken, where regression analysis showed that with the misting fan, Hot thermal neutrality can be obtained at a higher outdoor effective temperature (ET*). However, the Humid reduction in temperature comes at the expense of higher relative humidity which results in consistently greater biological (bacterial and fungal) pollutants being enumerated from samples collected under the misting fan system.
    [Show full text]
  • Clouds, Precipitation and Their Remote Sensing Intergovernmental
    25.09.12 Clouds, Precipitation and their Remote Sensing Prof. Susanne Crewell AG Integrated Remote Sensing Institute for Geophysics and Meteorology University of Cologne Susanne Crewell, Kompaktkurs, Jülich24. 25 September September 2012 2012 Intergovernmental Panel on Climate Change (IPCC) www.ipcc.ch Nobel price 2007 IPCC Fourth Assessment Report (FAR), 2007: "Warming of the climate system is unequivocal", and "Most of the observed increase in global average temperatures since the mid-20th century is very likely due to the observed increase in anthropogenic greenhouse gas concentrations". Aerosols, clouds and their interaction with climate is still the most uncertain area of climate change and require multidisciplinary coordinated research efforts. SusanneSusS sanna ne Crewell,Crewewellelll,K, Kompaktkurs,Kompakta kurs, JülichJülJüü ichchc 252 SeptemberSSeeptetetembembber 201220121 1 25.09.12 Why are clouds so complex? Cloud microphysical processes occur on small spatial scales and need to be parametrized in atmospheric models Cloud microphysics is strongly connected to other sub-grid scale processes (turbulence, radiation) Cloud droplets 0.01 mm diameter 100-1000 per cm3 Condensation nuclei Drizzle droplets 0.001 mm diameter 0.1 mm diameter 1000 per cm3 1 per cm3 Rain drops ca. 1 mm diameter, 1 drops per liter Susannesa Crewell, Kompaktkurs, Jülich 25 September 2012 Why are clouds so complex? From hydrometeors to single clouds to Einzelwolken to the global and cloud fields system Susanne Crewell, Kompaktkurs, Jülich 25 September
    [Show full text]
  • The Error Is the Feature: How to Forecast Lightning Using a Model Prediction Error [Applied Data Science Track, Category Evidential]
    The Error is the Feature: How to Forecast Lightning using a Model Prediction Error [Applied Data Science Track, Category Evidential] Christian Schön Jens Dittrich Richard Müller Saarland Informatics Campus Saarland Informatics Campus German Meteorological Service Big Data Analytics Group Big Data Analytics Group Offenbach, Germany ABSTRACT ACM Reference Format: Despite the progress within the last decades, weather forecasting Christian Schön, Jens Dittrich, and Richard Müller. 2019. The Error is the is still a challenging and computationally expensive task. Current Feature: How to Forecast Lightning using a Model Prediction Error: [Ap- plied Data Science Track, Category Evidential]. In Proceedings of 25th ACM satellite-based approaches to predict thunderstorms are usually SIGKDD Conference on Knowledge Discovery and Data Mining (KDD ’19). based on the analysis of the observed brightness temperatures in ACM, New York, NY, USA, 10 pages. different spectral channels and emit a warning if a critical threshold is reached. Recent progress in data science however demonstrates 1 INTRODUCTION that machine learning can be successfully applied to many research fields in science, especially in areas dealing with large datasets. Weather forecasting is a very complex and challenging task requir- We therefore present a new approach to the problem of predicting ing extremely complex models running on large supercomputers. thunderstorms based on machine learning. The core idea of our Besides delivering forecasts for variables such as the temperature, work is to use the error of two-dimensional optical flow algorithms one key task for meteorological services is the detection and pre- applied to images of meteorological satellites as a feature for ma- diction of severe weather conditions.
    [Show full text]
  • Operating Instructions Present Weather Sensor Parsivel
    Operating instructions Present Weather Sensor Parsivel English We reserve the right to make technical changes! Table of contents 1 Scope of delivery 5 2 Part numbers 5 3 Parsivel Factory Settings 6 4 Safety instructions 7 5 Introduction 8 5.1 Functional principle 8 5.2 Connection Options for the Parsivel 9 6 Installing the Parsivel 10 6.1 Cable Selection 10 6.2 Wiring the Parsivel 11 6.3 Grounding the Parsivel 13 6.4 Installing the Parsivel 14 7 Connecting the Parsivel to a data logger 15 7.1 Connecting the Parsivel to the LogoSens Station Manager via RS-485 interface 15 7.2 Connecting the Parsivel to a Data logger via the SDI-12 Interface 17 7.3 Connecting the Parsivel to a Data Logger with Impulse/Status Input 21 8 Connecting the Parsivel to a PC 23 8.1 Connecting the Parsivel to Interface Converter RS-485/RS-232 (Accessories) 23 8.2 Connecting the Parsivel to the ADAM-4520 Converter RS-485/RS-232 (Accessories) 25 8.3 Connecting the Parsivel to Interface Converter RS-485/USB (Accessories) 26 8.4 Connecting the Parsivel to any RS-485 Interface Converter 27 8.5 Connecting the Parsivel for configuration via the Service-Tool to a PC 27 9 Connecting the Parsivel to a Power Supply (Accessory) 29 10 Heating the Parsivel sensor heads 30 11 Operating Parsivel with a Terminal software 31 11.1 Set up communications between the Parsivel and the terminal program 31 11.2 Measured value numbers 32 11.3 Defining the formatting string 33 11.4 OTT telegram 33 11.5 Updating Parsivel Firmware 34 12 Maintenance 36 12.1 Cleaning the laser’s protective glass
    [Show full text]
  • 6.4 the Warning Time for Cloud-To-Ground Lightning in Isolated, Ordinary Thunderstorms Over Houston, Texas
    6.4 THE WARNING TIME FOR CLOUD-TO-GROUND LIGHTNING IN ISOLATED, ORDINARY THUNDERSTORMS OVER HOUSTON, TEXAS Nathan C. Clements and Richard E. Orville Texas A&M University, College Station, Texas 1. INTRODUCTION shear and buoyancy, with small magnitudes of vertical wind shear likely to produce ordinary, convective Lightning is a natural but destructive phenomenon storms. Weisman and Klemp (1986) describe the short- that affects various locations on the earth’s surface lived single cell storm as the most basic convective every year. Uman (1968) defines lightning as a self- storm. Therefore, this ordinary convective storm type will propagating atmospheric electrical discharge that results be the focus of this study. from the accumulation of positive and negative space charge, typically occurring within convective clouds. This 1.2 THUNDERSTORM CHARGE STRUCTURE electrical discharge can occur in two basic ways: cloud flashes and ground flashes (MacGorman and Rust The primary source of lightning is electric charge 1998, p. 83). The latter affects human activity, property separated in a cloud type known as a cumulonimbus and life. Curran et al. (2000) find that lightning is ranked (Cb) (Uman 1987). Interactions between different types second behind flash and river flooding as causing the of hydrometeors within a cloud are thought to carry or most deaths from any weather-related event in the transfer charges, thus creating net charge regions United States. From 1959 to 1994, there was an throughout a thunderstorm. Charge separation can average of 87 deaths per year from lightning. Curran et either come about by inductive mechanisms (i.e. al. also rank the state of Texas as third in the number of requires an electric field to induce charge on the surface fatalities from 1959 to 1994, behind Florida at number of the hydrometeor) or non-inductive mechanisms (i.e.
    [Show full text]
  • The Effect of Ownship Information and Nexrad Resolution on Pilot Decision Making in the Use of a Cockpit Weather Information Display
    NASA/CR-2001-210845 The Effect of Ownship Information and NexRad Resolution on Pilot Decision Making in the Use of a Cockpit Weather Information Display Paul F. Novacek, Malcolm A. Burgess, Michael L. Heck, and Alan F. Stokes RTI International, Hampton, Virginia December 2001 The NASA STI Program Office ... in Profile Since its founding, NASA has been dedicated to CONFERENCE PUBLICATION. Collected the advancement of aeronautics and space science. The NASA Scientific and Technical papers from scientific and technical conferences, symposia, seminars, or other Information (STI) Program Office plays a key meetings sponsored or co sponsored by part in helping NASA maintain this important NASA. role. SPECIAL PUBLICATION. Scientific, The NASA STI Program Office is operated by technical, or historical information from Langley Research Center, the lead center for NASA's scientific and technical information. The NASA programs, projects, and missions, often concerned with subjects having NASA STI Program Office provides access to the substantial public interest. NASA STI Database, the largest collection of aeronautical and space science STI in the world. The Program Office is also NASA's institutional TECHNICAL TRANSLATION. English language translations of foreign scientific mechanism for disseminating the results of its and technical material pertinent to NASA's research and development activities. These mission. results are published by NASA in the NASA STI Report Series, which includes the following report types: Specialized services that complement the STI Program Office's diverse offerings include TECHNICAL PUBLICATION. Reports of creating custom thesauri, building customized completed research or a major significant databases, organizing and publishing research phase of research that present the results of results ..
    [Show full text]
  • Imet-4 Radiosonde 403 Mhz GPS Synoptic
    iMet-4 Radiosonde 403 MHz GPS Synoptic Technical Data Sheet Temperature and Humidity Radiosonde Data Transmission The iMet-4 measures air temperature with a The iMet-4 radiosonde can transmit to an small glass bead thermistor. Its small size effective range of over 250 km*. minimizes effects caused by long and short- wave radiation and ensures fast response times. A 6 kHz peak-to-peak FM transmission maximizes efficiency and makes more channels The humidity sensor is a thin-film capacitive available for operational use. Seven frequency polymer that responds directly to relative selections are pre-programmed - with custom humidity. The sensor incorporates a temperature programming available. sensor to minimize errors caused by solar heating. Calibration Pressure and Height The iMet-4’s temperature and humidity sensors are calibrated using NIST traceable references to As recommended by GRUAN3, the iMet-4 is yield the highest data quality. equipped with a pressure sensor to calculate height at lower levels in the atmosphere. Once Benefits the radiosonde reaches the optimal height, pressure is derived using GPS altitude combined • Superior PTU performance with temperature and humidity data. • Lightweight, compact design • No assembly or recalibration required The pressure sensor facilitates the use of the • GRUAN3 qualified (pending) sonde in field campaigns where a calibrated • Status LED indicates transmit frequency barometer is not available to establish an selection and 3-D GPS solution accurate ground observation for GPS-derived • Simple one-button user interface pressure. For synoptic use, the sensor is bias adjusted at ground level. Winds Data from the radiosonde's GPS receiver is used to calculate wind speed and direction.
    [Show full text]
  • Lecture Notes on Marine Meteorology
    Lecture notes on Marine Meteorology By Shri S. P. Joshi Assistant. Meteorologist Office of DDGM (WF) India Meteorological Department Pune-5 Preface The aim of these lecture notes is to provide training to the marine observers in handling and maintenance of meteorological instruments and collect meteorological observations in the form of logbooks. The chapters included in these lecture notes are from the Basic and Intermediate training courses of the department. The present lecture notes are merely a collection of information available on Internet and are compiled from various WMO sites, freely available, keeping in view the up-and-coming trends and new technological advancements. This collection is for private circulation for trainees of Basic and Intermediate training courses of the department and the author do not intend to violate copyrights of anybody what so ever. Port Meteorological Officers in the immediate future have to deal with the modernization of the marine equipments and automation of Marine Data collection, its transmission and archival by observing minimum quality control through the in-built software like TURBOWIN. These lecture notes will also be useful to Port Meteorological Officers in understanding the nature of work of PMOs and will provide them the useful guidelines. A separate chapter on installation of Turbowin is also included in these notes. S. P. Joshi. 9th April 2005. Gudhi Padva Table of contents Chapter no Contents Page no. 1 WMO Voluntary Observing Ships’ Scheme 1 2 Meteorological Instrumentation on board ships 8 3 Port Meteorological Office ( PMO ) 15 4 The Ship Weather Code 19 5 Broadcast of weather bulletins for Merchant shipping 24 6 Broadcast of weather bulletins for Indian navy 28 7 Warnings to Ports and Storm Warning Signals 30 8 Broadcast of weather warnings for fishermen through 34 All India Radio.
    [Show full text]