BUFR Table D List of common sequences

Size: px
Start display at page:

Download "BUFR Table D List of common sequences"

Transcription

1 BUFR Table D List of common sequences F X Category of sequences Identifier NONE

2 Category 01 Location and identification sequences (Temperature and humidity instrumentation) Generic type of humidity instrument Configuration of sensors Type of shield or screen Horizontal width of screen or shield (x) Horizontal depth of screen or shield (y) Vertical height of screen or shield (z) Artificially ventilated screen or shield Amount of forced ventilation at time of reading (DRMM-II)

3 Category 04 Meteorological sequences common to satellite observations (2 May 2018) (BUFR sequence for describing satellites contributing to an observed geophysical quantity) Delayed replication of 8 descriptors Time significance = 28 Start of scan Year, month, day Hour, minute, second Time significance = 29 End of scan Year, month, day Hour, minute, second Satellite identifier Satellite instruments Time significance Set to missing (cancel) (CM-I)

4 Category 06 Meteorological or oceanographic sequences common to oceanographic observations (Chlorophyll-A (fluorescence) profile data) Delayed replication of 9 descriptors Extended delayed descriptor replication factor Gives number of depths Depth below sea/water surface Set to missing Qualifier for quality class Set to missing Set to missing Water pressure (DRMM-IV) Qualifier for quality class Set to 10 (pressure at a level) Fluorescence Chlorophyll-A In kg l-1 (= 109 mg m-3) Qualifier for quality class Set to 21 (Chlorophyll-A at a level) (Dissolved nitrate profile data) (DRMM-IV) Delayed replication of 9 descriptors Extended delayed descriptor replication factor Number of depths Depth below sea/water surface Set to missing Qualifier for quality class Set to missing Set to missing Water pressure Qualifier for quality class Set to 10 (pressure at a level) Dissolved nitrate In μmol kg Qualifier for quality class Set to 22 (nitrate at a level) (ph profile data) (DRMM-IV) Delayed replication of 9 descriptors Extended delayed descriptor replication factor Number of depths Depth below sea/water surface Set to missing Qualifier for quality class Set to missing Set to missing Water pressure Qualifier for quality class Set to 10 (pressure at a level) ph scale ph Dimensionless Qualifier for quality class Set to 23 (ph at a level) (Backscatter profile data) (DRMM-IV) Spectrographic wavelength In m Delayed replication of 9 descriptors Extended delayed descriptor replication factor Number of depths Depth below sea/water surface Set to missing Qualifier for quality class Set to missing Set to missing Water pressure

5 Qualifier for quality class Set to 10 (pressure at a level) Backscattering m Qualifier for quality class Set to 24 (backscatter at a level)

6 Category 07 Surface report sequences (land) WIGOS identifier (BUFR template for surface observations from n-minute period) Station or site name Type of station Year, month, day Hour, minute Station identification, time, horizontal and vertical coordinates Latitude/longitude (high accuracy) Height of station ground above mean sea level Height of barometer above mean sea level Observation sequence number Pressure Pressure Pressure reduced to mean sea level Pressure (standard level) Geopotential height of the standard level Wind Delayed replication of 18 descriptors Height of sensor above local ground (or deck of marine platform) Type of instrumentation for wind measurement Time significance = 2 Time averaged (CM-I) Time period or displacement = -10 minutes, or number of minutes after a significant change of wind Wind direction Wind speed Time significance Set to missing Maximum wind gust direction Maximum wind gust speed Extreme counterclockwise wind direction of a variable wind Extreme clockwise wind direction of a variable wind Time period or displacement = 0 minutes Temperature and humidity data Delayed replication of 11 descriptors Height of sensor above local ground (or deck of marine platform) Surface qualifier (temperature data) Temperature/air temperature Scale Dewpoint temperature Scale 2

7 Relative humidity Original measured value Relative humidity Height of sensor above local ground (or deck of Set to missing (cancel) marine platform) Surface qualifier (temperature data) Set to missing (cancel) Soil temperature and soil moisture Delayed replication of 7 descriptors Depth below land surface Soil temperature Soil moisture Depth below land surface Set to missing (cancel) Visibility Delayed replication of 7 descriptors Height of sensor above local ground (or deck of marine platform) Attribute of following value (2 May 2018) Horizontal visibility Or, (Meteorological optical range) Height of sensor above local ground (or deck of Set to missing (cancel) marine platform) Cloud Delayed replication of 2 descriptors Cloud data Vertical significance (surface observations) Set to missing Ice and State of the ground Delayed replication of 5 descriptors Ice deposit (thickness) Rate of ice accretion (estimated) Delayed replication of 4 descriptors State of ground and snow depth measurement Present weather Delayed replication of 14 descriptors Time period or displacement = - n minutes Present weather

8 Time increment = -n minutes Time period or displacement = -1 minutes Short time increment = 1 minutes Delayed replication of 4 descriptors n Present weather Precipitation Delayed replication of 2 descriptors Precipitation measurement Height of sensor above local ground (or deck of Set to missing (cancel) marine platform) Evaporation Delayed replication of 1 descriptor Evaporation measurement Sunshine and radiation Delayed replication of 1 descriptor Total sunshine data Delayed replication of 1 descriptor Radiation data Lightning Delayed replication of 5 descriptors Time period or displacement = -n minutes Number of flashes (thunderstorm)

9 Category 08 Surface report sequences (sea) NONE

10 Category 09 Vertical sounding sequences (conventional data) WIGOS identifier (Sequence for representation of radiosonde descent data) Radiosonde type Solar and infrared radiation correction Tracking technique/status of system used Type of measuring equipment used Additional information on radiosonde ascent Valid also for decent Date/time of launch Coordinates significance = 2 Start of observation Latitude/longitude (high accuracy) (CM-I) Height Begin of descending of radiosonde above mean sea level Coordinates significance Set to missing (cancel) Delayed replication of 1 descriptor Extended delayed descriptor replication factor Temperature, dewpoint and wind data at a pressure level with radiosonde position Delayed replication of 1 descriptor Wind shear data at a pressure level with radiosonde position

11 Category 10 Vertical sounding sequences (satellite data) NONE

BUFR Table D - List of common sequences

BUFR Table D - List of common sequences BUFR Table D - List of common sequences Category of sequences 3 00 BUFR table entries sequences 3 01 Location and identification sequences 3 02 Meteorological sequences common to surface data 3 03 Meteorological

More information

CREX Table D List of common sequences

CREX Table D List of common sequences Ver. 31.0.0 7 November 2018 CREX Table D List of common sequences Category of sequences D 00 CREX table entries sequences D 01 Location and identification sequences D 02 Meteorological sequences common

More information

LIST OF AMENDMENTS TO MANUAL ON CODES

LIST OF AMENDMENTS TO MANUAL ON CODES LIST OF AMENDMENTS TO MANUAL ON CODES PRE-OPERATIONAL CONTENTS I. FM 92 GRIB NONE II. FM 94 /FM 95 1. Sequence for synoptic reports from sea stations suitable for VOS observation data (editorial changes)

More information

AWS BUFR representation of nominal values

AWS BUFR representation of nominal values WORLD METEOROLOGICAL ORGANIZATION COMMISSION FOR BASIC SYSTEMS OPEN PROGRAMME AREA GROUP ON INTEGRATED OBSERVING SYSTEMS EXPERT TEAM ON REQUIREMENTS FOR DATA FROM AUTOMATIC WEATHER STATIONS FOURTH SESSION

More information

LIST OF AMENDMENTS TO MANUAL ON CODES

LIST OF AMENDMENTS TO MANUAL ON CODES LIST OF AMENDMENTS TO MANUAL ON CODES FAST-TRACK 2016-1 (4 May 2016) CONTENTS Part B Binary Codes b. List of binary codes with their specifications and associated code tables I. FM 92 GRIB General regularly

More information

BUFR format in a nutshell

BUFR format in a nutshell BUFR format in a nutshell Enrico Fucile Enrico.Fucile@ecmwf.int ECMWF February 19, 2018 WMO Binary Codes BUFR (Binary Universal Form for the Representation of meteorological data) is a flexible binary

More information

BUFR/CREX Table B Classification of elements

BUFR/CREX Table B Classification of elements Ver. 29.0.0 8 November 2017 FM 94, FM 95 TABLES RELATIVE TO SECTION 3 / Table B Classification of elements F X Class Comments 0 00 / table entries 0 01 Identification Identifies origin and type of data

More information

BUFR TABLES RELATIVE TO SECTION 3. BUFR Table B Classification of elements

BUFR TABLES RELATIVE TO SECTION 3. BUFR Table B Classification of elements S RELATIVE TO SECTION 3 Table B Classification of elements F X Class Comments 0 00 table entries 0 01 Identification Identifies origin and type of data 0 02 Instrumentation Defines instrument types used

More information

F O U N D A T I O N A L C O U R S E

F O U N D A T I O N A L C O U R S E F O U N D A T I O N A L C O U R S E December 6, 2018 Satellite Foundational Course for JPSS (SatFC-J) F O U N D A T I O N A L C O U R S E Introduction to Microwave Remote Sensing (with a focus on passive

More information

WORLD METEOROLOGICAL ORGANIZATION THE WMO TABLE DRIVEN CODES: THE 21 ST CENTURY UNIVERSAL OBSERVATION CODES

WORLD METEOROLOGICAL ORGANIZATION THE WMO TABLE DRIVEN CODES: THE 21 ST CENTURY UNIVERSAL OBSERVATION CODES WORLD METEOROLOGICAL ORGANIZATION THE WMO TABLE DRIVEN CODES: THE 21 ST CENTURY UNIVERSAL OBSERVATION CODES 1 THE WMO TABLE DRIVEN CODES: THE 21 ST CODES CENTURY UNIVERSAL OBSERVATION ABSTRACT The table

More information

BUFR/CREX Table B - Classification of elements

BUFR/CREX Table B - Classification of elements - ver. 18.0.0 TABLES RELATIVE TO SECTION 3 / Table B - Classification of elements F X Class Comments 0 00 / table entries 0 01 Identification Identifies origin and type of data 0 02 Instrumentation Defines

More information

THE METEOROLOGICAL DATA QUALITY MANAGEMENT OF THE ROMANIAN NATIONAL SURFACE OBSERVATION NETWORK

THE METEOROLOGICAL DATA QUALITY MANAGEMENT OF THE ROMANIAN NATIONAL SURFACE OBSERVATION NETWORK THE METEOROLOGICAL DATA QUALITY MANAGEMENT OF THE ROMANIAN NATIONAL SURFACE OBSERVATION NETWORK Ioan Ralita, Ancuta Manea, Doina Banciu National Meteorological Administration, Romania Ionel Dragomirescu

More information

CGMS Baseline. Sustained contributions to the Global Observing System. Endorsed by CGMS-46 in Bengaluru, June 2018

CGMS Baseline. Sustained contributions to the Global Observing System. Endorsed by CGMS-46 in Bengaluru, June 2018 CGMS Baseline Sustained contributions to the Global Observing System Best Practices for Achieving User Readiness for New Meteorological Satellites Endorsed by CGMS-46 in Bengaluru, June 2018 CGMS/DOC/18/1028862,

More information

Climate & Earth System Science. Introduction to Meteorology & Climate. Chapter 05 SOME OBSERVING INSTRUMENTS. Instrument Enclosure.

Climate & Earth System Science. Introduction to Meteorology & Climate. Chapter 05 SOME OBSERVING INSTRUMENTS. Instrument Enclosure. Climate & Earth System Science Introduction to Meteorology & Climate MAPH 10050 Peter Lynch Peter Lynch Meteorology & Climate Centre School of Mathematical Sciences University College Dublin Meteorology

More information

Weather vs. Climate. Tucson NWS homepage:

Weather vs. Climate. Tucson NWS homepage: Weather vs. Climate Tucson NWS homepage: www.nws.noaa.gov/twc/ A Weather Forecaster? Betty claims to know exactly when it s going to rain because her knee starts to hurt. Ms. Betty Martin of Newburgh,

More information

Temperature (T) degrees Celsius ( o C) arbitrary scale from 0 o C at melting point of ice to 100 o C at boiling point of water Also (Kelvin, K) = o C

Temperature (T) degrees Celsius ( o C) arbitrary scale from 0 o C at melting point of ice to 100 o C at boiling point of water Also (Kelvin, K) = o C 1 2 3 4 Temperature (T) degrees Celsius ( o C) arbitrary scale from 0 o C at melting point of ice to 100 o C at boiling point of water Also (Kelvin, K) = o C plus 273.15 0 K is absolute zero, the minimum

More information

REVISION OF THE STATEMENT OF GUIDANCE FOR GLOBAL NUMERICAL WEATHER PREDICTION. (Submitted by Dr. J. Eyre)

REVISION OF THE STATEMENT OF GUIDANCE FOR GLOBAL NUMERICAL WEATHER PREDICTION. (Submitted by Dr. J. Eyre) WORLD METEOROLOGICAL ORGANIZATION Distr.: RESTRICTED CBS/OPAG-IOS (ODRRGOS-5)/Doc.5, Add.5 (11.VI.2002) COMMISSION FOR BASIC SYSTEMS OPEN PROGRAMME AREA GROUP ON INTEGRATED OBSERVING SYSTEMS ITEM: 4 EXPERT

More information

MxVision WeatherSentry Web Services Content Guide

MxVision WeatherSentry Web Services Content Guide MxVision WeatherSentry Web Services Content Guide July 2014 DTN 11400 Rupp Drive Minneapolis, MN 55337 00.1.952.890.0609 This document and the software it describes are copyrighted with all rights reserved.

More information

Guidelines on Quality Control Procedures for Data from Automatic Weather Stations

Guidelines on Quality Control Procedures for Data from Automatic Weather Stations Guidelines on Quality Control Procedures for Data from Automatic Weather Stations Igor Zahumenský Slovak Hydrometeorological Institute SHMI, Jeséniova 17, 833 15 Bratislava, Slovakia Tel./Fax. +421 46

More information

CGMS Baseline In response to CGMS action/recommendation A45.01 HLPP reference: 1.1.8

CGMS Baseline In response to CGMS action/recommendation A45.01 HLPP reference: 1.1.8 Prepared by WGIII Agenda Item: 7.1 Discussed in WGIII CGMS Baseline In response to CGMS action/recommendation A45.01 HLPP reference: 1.1.8 In CGMS-45, Working Group III agreed to hold a review of the CGMS

More information

World Meteorological Organization Organisation météorologique mondiale Organizaci6n Meteorol6gica Mundial BceMHpHan MeTeoponorHYecKan oprahh3al..

World Meteorological Organization Organisation météorologique mondiale Organizaci6n Meteorol6gica Mundial BceMHpHan MeTeoponorHYecKan oprahh3al.. WMOOMM Our ref.: World Meteorological Organization Organisation météorologique mondiale Organizaci6n Meteorol6gica Mundial BceMHpHan MeTeoponorHYecKan oprahh3al..\hn ~I..1~.;)U 4.:J.WI d...j:.:j.1 1!t~S\~filffi

More information

Observational Needs for Polar Atmospheric Science

Observational Needs for Polar Atmospheric Science Observational Needs for Polar Atmospheric Science John J. Cassano University of Colorado with contributions from: Ed Eloranta, Matthew Lazzara, Julien Nicolas, Ola Persson, Matthew Shupe, and Von Walden

More information

Unit: Weather Study Guide

Unit: Weather Study Guide Name: Period: Unit: Weather Study Guide Define each vocabulary word on a separate piece of paper or index card. Weather Climate Temperature Wind chill Heat index Sky conditions UV index Visibility Wind

More information

Chapter 12 Section 12.1 The causes of weather

Chapter 12 Section 12.1 The causes of weather Chapter 12 Section 12.1 The causes of weather Main Idea: Air masses have different temperatures and amounts of moisture because of the uneven heating of earth's surface. What is Meteorology The study of

More information

Chapter 12: Meteorology

Chapter 12: Meteorology Chapter 12: Meteorology Section 1: The Causes of Weather 1. Compare and contrast weather and climate. 2. Analyze how imbalances in the heating of Earth s surface create weather. 3. Describe how and where

More information

Series tore word. Acknowledgements

Series tore word. Acknowledgements Series tore word p. xi Preface p. xiii Acknowledgements p. xv Disclaimer p. xvii Introduction p. 1 The instrumental age p. 2 Measurements and the climate record p. 2 Clouds and rainfall p. 3 Standardisation

More information

Study Guide. Earth Systems 1109 Weather Dynamics. Adult Basic Education Science. Prerequisites: Credit Value: 1

Study Guide. Earth Systems 1109 Weather Dynamics. Adult Basic Education Science. Prerequisites: Credit Value: 1 Adult Basic Education Science Weather Dynamics Study Guide Prerequisites: None Credit Value: 1 Text: Science 10 ; Ritter, Plumb, et al; Nelson, 2001. Earth Systems Concentration Earth Systems 3109A Earth

More information

NATS 101 Section 13: Lecture 3. Weather vs. Climate

NATS 101 Section 13: Lecture 3. Weather vs. Climate NATS 101 Section 13: Lecture 3 Weather vs. Climate Definition of Weather Weather: Condition of the atmosphere at a particular time and place. Comprised of: Air temperature: Degree of hotness or coldness

More information

BUFR Reference Manual

BUFR Reference Manual BUFR Reference Manual Milan Dragosavac Operations Department August 2008 c Copyright 2008 European Centre for Medium-Range Weather Forecasts Shinfield Park, Reading, RG2 9AX, United Kingdom Literary and

More information

AMENDMENTS TO THE MANUAL ON CODES (WMO-NO. 306)

AMENDMENTS TO THE MANUAL ON CODES (WMO-NO. 306) AMENDMENTS TO THE MANUAL ON CODES (WMO-NO. 306) FAST-TRACK 2016-2 (2 November 2016) CONTENTS Part B Binary Codes b. List of binary codes with their specifications and associated code tables I. FM 92 GRIB

More information

Remote Sensing in Meteorology: Satellites and Radar. AT 351 Lab 10 April 2, Remote Sensing

Remote Sensing in Meteorology: Satellites and Radar. AT 351 Lab 10 April 2, Remote Sensing Remote Sensing in Meteorology: Satellites and Radar AT 351 Lab 10 April 2, 2008 Remote Sensing Remote sensing is gathering information about something without being in physical contact with it typically

More information

Unit 5 Lesson 3 How is Weather Predicted? Copyright Houghton Mifflin Harcourt Publishing Company

Unit 5 Lesson 3 How is Weather Predicted? Copyright Houghton Mifflin Harcourt Publishing Company Tracking the Weather Warm up 1 Why is it important to watch the weather forecast before traveling to another country? Tracking the Weather A meteorologist is a scientist who studies weather. Meteorologists

More information

VISION FOR THE GOS IN 2025 ( Approved by CBS-XIV and Adopted by EC LXI in June 2009)

VISION FOR THE GOS IN 2025 ( Approved by CBS-XIV and Adopted by EC LXI in June 2009) WORLD METEOROLOGICAL ORGANIZATION Weather Climate Water VISION FOR THE GOS IN 2025 ( Approved by CBS-XIV and Adopted by EC LXI in June 2009) PREAMBLE This Vision provides high-level goals to guide the

More information

2 nd Cryonet-Asia Worskshop Salekhard, Russian Federation (2-5 February 2016)

2 nd Cryonet-Asia Worskshop Salekhard, Russian Federation (2-5 February 2016) WMO 2 nd Cryonet-Asia Worskshop Salekhard, Russian Federation (2-5 February 2016) WMO Rolling Review of Requirements (RRR) Etienne Charpentier Chief, WMO Observing Systems Division WMO; Name of Department

More information

DSJRA-55 Product Users Handbook. Climate Prediction Division Global Environment and Marine Department Japan Meteorological Agency July 2017

DSJRA-55 Product Users Handbook. Climate Prediction Division Global Environment and Marine Department Japan Meteorological Agency July 2017 DSJRA-55 Product Users Handbook Climate Prediction Division Global Environment and Marine Department Japan Meteorological Agency July 2017 Change record Version Date Remarks 1.0 13 July 2017 First version

More information

Go With the Flow From High to Low Investigating Isobars

Go With the Flow From High to Low Investigating Isobars Go With the Flow From High to Low Investigating Isobars Science 10 Mrs. Purba Air Masses The air over a warm surface can be heated, causing it to rise above more dense air. The result is the formation

More information

Meteorology. I. The Atmosphere - the thin envelope of gas that surrounds the earth.

Meteorology. I. The Atmosphere - the thin envelope of gas that surrounds the earth. Meteorology I. The Atmosphere - the thin envelope of gas that surrounds the earth. A. Atmospheric Structure - the atmosphere is divided into five distinct layers that are based on their unique characteristics.

More information

Lecture 4: Meteorological Satellites and Instruments. Acknowledgement: Dr. S. Kidder at Colorado State Univ.

Lecture 4: Meteorological Satellites and Instruments. Acknowledgement: Dr. S. Kidder at Colorado State Univ. Lecture 4: Meteorological Satellites and Instruments Acknowledgement: Dr. S. Kidder at Colorado State Univ. Homework for the Spring Break: get some tangible, preliminary results for your final project.

More information

Introduction. Sunny Partly Cloudy Cloudy. Flurries Snow Ice. Showers Thunderstorms Rain. High Pressure Low Pressure FRONTS. Cold Warm Stationary

Introduction. Sunny Partly Cloudy Cloudy. Flurries Snow Ice. Showers Thunderstorms Rain. High Pressure Low Pressure FRONTS. Cold Warm Stationary Introduction Weather can change from minute to minute, hour to hour, day to day, or season to season. Meteorologists are scientists who study Earth s atmosphere in order to predict these changes. Meteorologists

More information

Science Olympiad Meteorology Quiz #1 Page 1 of 7

Science Olympiad Meteorology Quiz #1 Page 1 of 7 1) What is generally true about the stratosphere: a) Has turbulent updrafts and downdrafts. b) Has either a stable or increasing temperature profile with altitude. c) Where the auroras occur. d) Both a)

More information

Recent Improvement of Integrated Observation Systems in JMA

Recent Improvement of Integrated Observation Systems in JMA Recent Improvement of Integrated Observation Systems in JMA Mr Osamu Suzuki and Mr Yoshihiko Tahara Japan Meteorological Agency 1-3-4 Otemachi, Chiyoda-ku, Tokyo 100-8122, Japan Tel: +81-3-3212-8341, Fax:

More information

The Causes of Weather

The Causes of Weather Meteorology The Causes of Weather Where does the weather in our country come from? * Which air masses determine the weather in our country? * Weather or Climate? *The current state of the atmosphere *

More information

Land Surface Temperature Measurements From the Split Window Channels of the NOAA 7 Advanced Very High Resolution Radiometer John C.

Land Surface Temperature Measurements From the Split Window Channels of the NOAA 7 Advanced Very High Resolution Radiometer John C. Land Surface Temperature Measurements From the Split Window Channels of the NOAA 7 Advanced Very High Resolution Radiometer John C. Price Published in the Journal of Geophysical Research, 1984 Presented

More information

Michael F. Stringfellow

Michael F. Stringfellow Michael F. Stringfellow Thermals Columns or bubbles of warm air that rise from the ground when it is heated by the sun Soaring Sustained engineless flight using natural sources of lift Boundary or mixing

More information

Weather Report. PCAS Camp 2009/10. By Chris Mckenzie

Weather Report. PCAS Camp 2009/10. By Chris Mckenzie Weather Report PCAS Camp 2009/10 By Chris Mckenzie Abstract An AWS (Automatic Weather Station) was set up at PCAS camp, located on the Ross Ice Shelf in the Windless Bight (figure 1). Data was measured

More information

EUMETSAT STATUS AND PLANS

EUMETSAT STATUS AND PLANS 1 EUM/TSS/VWG/15/826793 07/10/2015 EUMETSAT STATUS AND PLANS François Montagner, Marine Applications Manager, EUMETSAT WMO Polar Space Task Group 5 5-7 October 2015, DLR, Oberpfaffenhofen PSTG Strategic

More information

National Maritime Center

National Maritime Center National Maritime Center Providing Credentials to Mariners (Sample Examination) Page 1 of 5 Choose the best answer to the following Multiple Choice Questions. 1. Fog is formed when which condition exists?

More information

Page 1. Name:

Page 1. Name: Name: 1) As the difference between the dewpoint temperature and the air temperature decreases, the probability of precipitation increases remains the same decreases 2) Which statement best explains why

More information

What are Aerosols? Suspension of very small solid particles or liquid droplets Radii typically in the range of 10nm to

What are Aerosols? Suspension of very small solid particles or liquid droplets Radii typically in the range of 10nm to What are Aerosols? Suspension of very small solid particles or liquid droplets Radii typically in the range of 10nm to 10µm Concentrations decrease exponentially with height N(z) = N(0)exp(-z/H) Long-lived

More information

Passage (click here to show all)

Passage (click here to show all) Passage (click here to show all) Use the information in the table and maps below to answer questions #-##. Weather Table and Maps The weather information shown below was reported on Sunday, the 15th of

More information

Atmospheric Processes

Atmospheric Processes Atmospheric Processes Atmospheric prognostic variables Wind Temperature Humidity Cloud Water/Ice Atmospheric processes Mixing Radiation Condensation/ Evaporation Precipitation Surface exchanges Friction

More information

Chapter Introduction. Weather. Patterns. Forecasts Chapter Wrap-Up

Chapter Introduction. Weather. Patterns. Forecasts Chapter Wrap-Up Chapter Introduction Lesson 1 Lesson 2 Lesson 3 Describing Weather Weather Patterns Weather Forecasts Chapter Wrap-Up How do scientists describe and predict weather? What do you think? Before you begin,

More information

RF Propagation Characteristics on Leg 1 of July 06 OC3570 Cruise: Comparison of cruise sounding data, climatology and model data.

RF Propagation Characteristics on Leg 1 of July 06 OC3570 Cruise: Comparison of cruise sounding data, climatology and model data. RF Propagation Characteristics on Leg 1 of July 06 OC3570 Cruise: Comparison of cruise sounding data, climatology and model data. LCDR Bob Jones Introduction and Background The purpose of this project

More information

Ch. 3: Weather Patterns. Sect. 1: Air Mass & Fronts Sect. 2: Storms Sect. 3: Predicting the Weather

Ch. 3: Weather Patterns. Sect. 1: Air Mass & Fronts Sect. 2: Storms Sect. 3: Predicting the Weather Ch. 3: Weather Patterns Sect. 1: Air Mass & Fronts Sect. 2: Storms Sect. 3: Predicting the Weather Sect. 1: Air Masses & Fronts An air mass is a huge body of air that has similar temperature, humidity,

More information

a. Air is more dense b. Associated with cold air (more dense than warm air) c. Associated with sinking air

a. Air is more dense b. Associated with cold air (more dense than warm air) c. Associated with sinking air Meteorology 1. Air pressure the weight of air pressing down on Earth 2. Temperature and altitude determine air pressure 3. The more air particles are present, the more air density or pressure exists 4.

More information

25.1 Air Masses. Section 25.1 Objectives

25.1 Air Masses. Section 25.1 Objectives Section 25.1 Objectives Explain how an air mass forms. List the four main types of air masses. Describe how air masses affect the weather of North America. Air Masses 25.1 Air Masses Differences in air

More information

Observing Weather: Making the Invisible Visible. Dr. Michael J. Passow

Observing Weather: Making the Invisible Visible. Dr. Michael J. Passow Observing Weather: Making the Invisible Visible Dr. Michael J. Passow What Is Weather? Weather refers to the conditions of the atmosphere at a certain place and time. Weather differs from Climate, which

More information

Annex 1 to Recommendation 9 (JCOMM-III)

Annex 1 to Recommendation 9 (JCOMM-III) Annex 1 to Recommendation 9 (JCOMM-III) AMENDMENTS TO THE MANUAL ON MARINE METEOROLOGICAL SERVICES (WMO-No. 558) AND GUIDE TO MARINE METEOROLOGICAL SERVICES (WMO-No. 471) LAYOUT FOR THE INNATIONAL MARITIME

More information

DANO, Burkina Faso. Instruments Data set Status Highlights. Norbert Kalthoff and Juliane Schwendike. Institut für Meteorologie und Klimaforschung

DANO, Burkina Faso. Instruments Data set Status Highlights. Norbert Kalthoff and Juliane Schwendike. Institut für Meteorologie und Klimaforschung DANO, Burkina Faso Instruments Data set Status Highlights by Norbert Kalthoff and Juliane Schwendike Dano (super-)site in Burkina Faso Dreyer Foundation Dano Dano Bontioli Measurements at Bontioli site

More information

MASTERY ASSIGNMENT 2015

MASTERY ASSIGNMENT 2015 Climate & Meteorology MASTERY ASSIGNMENT 2015 Directions: You must submit this document via Google Docs to lzimmerman@wcpss.net. The document must include the questions and pictures must be hand drawn

More information

Assimilation of satellite derived soil moisture for weather forecasting

Assimilation of satellite derived soil moisture for weather forecasting Assimilation of satellite derived soil moisture for weather forecasting www.cawcr.gov.au Imtiaz Dharssi and Peter Steinle February 2011 SMOS/SMAP workshop, Monash University Summary In preparation of the

More information

4 Forecasting Weather

4 Forecasting Weather CHAPTER 2 4 Forecasting Weather SECTION Understanding Weather BEFORE YOU READ After you read this section, you should be able to answer these questions: What instruments are used to forecast weather? How

More information

Assimilation of ASCAT soil wetness

Assimilation of ASCAT soil wetness EWGLAM, October 2010 Assimilation of ASCAT soil wetness Bruce Macpherson, on behalf of Imtiaz Dharssi, Keir Bovis and Clive Jones Contents This presentation covers the following areas ASCAT soil wetness

More information

BUFR Reference Manual

BUFR Reference Manual BUFR Reference Manual Milan Dragosavac Operations Department January 2004 c Copyright 2004 European Centre for Medium-Range Weather Forecasts Shinfield Park, Reading, RG2 9AX, United Kingdom Literary and

More information

CHAPTER 13 WEATHER ANALYSIS AND FORECASTING MULTIPLE CHOICE QUESTIONS

CHAPTER 13 WEATHER ANALYSIS AND FORECASTING MULTIPLE CHOICE QUESTIONS CHAPTER 13 WEATHER ANALYSIS AND FORECASTING MULTIPLE CHOICE QUESTIONS 1. The atmosphere is a continuous fluid that envelops the globe, so that weather observation, analysis, and forecasting require international

More information

London Heathrow Field Site Metadata

London Heathrow Field Site Metadata London Heathrow Field Site Metadata Field Site Information Name: Heathrow src_id (Station ID number): 708 Geographic Area: Greater London Latitude (decimal ): 51.479 Longitude (decimal ): -0.449 OS Grid

More information

National Climatic Data Center DATA DOCUMENTATION FOR DATA SET 6406 (DSI-6406) ASOS SURFACE 1-MINUTE, PAGE 2 DATA. July 12, 2006

National Climatic Data Center DATA DOCUMENTATION FOR DATA SET 6406 (DSI-6406) ASOS SURFACE 1-MINUTE, PAGE 2 DATA. July 12, 2006 DATA DOCUMENTATION FOR DATA SET 6406 (DSI-6406) ASOS SURFACE 1-MINUTE, PAGE 2 DATA July 12, 2006 151 Patton Ave. Asheville, NC 28801-5001 USA Table of Contents Topic Page Number 1. Abstract... 3 2. Element

More information

Wind direction measures in degrees Occasion described with codes, when is calm or variable wind. Explanation

Wind direction measures in degrees Occasion described with codes, when is calm or variable wind. Explanation Introduction The searching results explanations of meteorological data Depending on the parameter, the instrumental measuring or visual observation method is used for the meteorological observations. Instrumentally

More information

7. The weather instrument below can be used to determine relative humidity.

7. The weather instrument below can be used to determine relative humidity. 1. What is the dewpoint temperature when the dry-bulb temperature is 12 C and the wet-bulb temperature is 7 C? A) 1 C B) -2 C C) -5 C D) 4 C 2. A parcel of air has a dry-bulb temperature reading of 16

More information

4 Forecasting Weather

4 Forecasting Weather CHAPTER 16 4 Forecasting Weather SECTION Understanding Weather BEFORE YOU READ After you read this section, you should be able to answer these questions: What instruments are used to forecast weather?

More information

HY-2A Satellite User s Guide

HY-2A Satellite User s Guide National Satellite Ocean Application Service 2013-5-16 Document Change Record Revision Date Changed Pages/Paragraphs Edit Description i Contents 1 Introduction to HY-2 Satellite... 1 2 HY-2 satellite data

More information

5.1 Use of the Consensus Reference Concept for Testing Radiosondes. Joe Facundo and Jim Fitzgibbon, Office of Operational Systems,

5.1 Use of the Consensus Reference Concept for Testing Radiosondes. Joe Facundo and Jim Fitzgibbon, Office of Operational Systems, 5. Use of the Consensus Reference Concept for Testing Radiosondes Joe Facundo and Jim Fitzgibbon, Office of Operational Systems, Silver Spring, Maryland and Sterling, Virginia. INTRODUCTION The U. S. has

More information

Day Snow-Fog RGB Detection of low-level clouds and snow/ice covered area

Day Snow-Fog RGB Detection of low-level clouds and snow/ice covered area JMA Day Snow-Fog RGB Detection of low-level clouds and snow/ice covered area Meteorological Satellite Center, JMA What s Day Snow-Fog RGB? R : B04 (N1 0.86) Range : 0~100 [%] Gamma : 1.7 G : B05 (N2 1.6)

More information

- satellite orbits. Further Reading: Chapter 04 of the text book. Outline. - satellite sensor measurements

- satellite orbits. Further Reading: Chapter 04 of the text book. Outline. - satellite sensor measurements (1 of 12) Further Reading: Chapter 04 of the text book Outline - satellite orbits - satellite sensor measurements - remote sensing of land, atmosphere and oceans (2 of 12) Introduction Remote Sensing:

More information

Development of Innovative Technology to Provide Low-Cost Surface Atmospheric Observations in Data-sparse Regions

Development of Innovative Technology to Provide Low-Cost Surface Atmospheric Observations in Data-sparse Regions Development of Innovative Technology to Provide Low-Cost Surface Atmospheric Observations in Data-sparse Regions Paul Kucera and Martin Steinson University Corporation for Atmospheric Research/COMET 3D-Printed

More information

Migration from TAC to BUFR for TEMP observations

Migration from TAC to BUFR for TEMP observations Migration from TAC to BUFR for TEMP observations Mohamed Anis Satouri, December 2017 National Institute of Meteorology, Tunisia anissatouri@gmail.com In collaboration with Alena Trojakova Czech Hydrometeorological

More information

METEOSAT THIRD GENERATION

METEOSAT THIRD GENERATION METEOSAT THIRD GENERATION FACTS AND FIGURES MONITORING WEATHER AND CLIMATE FROM SPACE A HIGHLY INNOVATIVE GEOSTATIONARY SATELLITE SYSTEM FOR EUROPE AND AFRICA The Meteosat Third Generation (MTG) system

More information

Weather Unit Part 2: Meteorology

Weather Unit Part 2: Meteorology Name: Earth Science Date: Period: Weather Unit Part 2: Meteorology 1 The map below shows North America and its surrounding bodies of water. Country borders are shown. On the map, label the following locations:

More information

Weather Maps. Name:& & &&&&&Advisory:& & 1.! A&weather&map&is:& & & & 2.! Weather&fronts&are:& & & & & &

Weather Maps. Name:& & &&&&&Advisory:& & 1.! A&weather&map&is:& & & & 2.! Weather&fronts&are:& & & & & & Name: Advisory: Weather Maps 1. Aweathermapis: 2. Weatherfrontsare: a. Labelthefrontsbelow: 1. 2. 3. 4. 3. Clovercoversymbols 4. Precipitationsymbols 5. 6. 7. 8. 5. RadarEchoIntensityshows 6. Isobarsare

More information

for JMA/WMO Training Workshop on CALIBRATION AND MAINTENANCE OF METEOROLOGICAL INSTRUMENTS

for JMA/WMO Training Workshop on CALIBRATION AND MAINTENANCE OF METEOROLOGICAL INSTRUMENTS for JMA/WMO Training Workshop on CALIBRATION AND MAINTENANCE OF METEOROLOGICAL INSTRUMENTS in RA II (ASIA) 0. Overview of JMA 3 4 1. Surface observation station 5-8 2. Instruments in operational use 9-14

More information

WATER IN THE ATMOSPHERE

WATER IN THE ATMOSPHERE WATER IN THE ATMOSPHERE During a rainstorm, the air feels moist On a clear, cloudless day, the air may feel dry As the sun heats the land and oceans, the amount of water in the atmosphere changes Water

More information

Weather - is the state of the atmosphere at a specific time & place

Weather - is the state of the atmosphere at a specific time & place Weather Section 1 Weather - is the state of the atmosphere at a specific time & place Includes such conditions as air pressure, wind, temperature, and moisture in the air The Sun s heat evaporates water

More information

National Maritime Center

National Maritime Center National Maritime Center Providing Credentials to Mariners (Sample Examination) Page 1 of 5 Choose the best answer to the following Multiple Choice Questions. 1. In a weather report, the term "visibility"

More information

III. Section 3.3 Vertical air motion can cause severe storms

III. Section 3.3 Vertical air motion can cause severe storms III. Section 3.3 Vertical air motion can cause severe storms http://www.youtube.com/watch?v=nxwbr60tflg&feature=relmfu A. Thunderstorms form from rising moist air Electrical charges build up near the tops

More information

Xinhua Liu National Meteorological Center (NMC) of China Meteorological Administration (CMA)

Xinhua Liu National Meteorological Center (NMC) of China Meteorological Administration (CMA) The short-time forecasting and nowcasting technology of severe convective weather for aviation meteorological services in China Xinhua Liu National Meteorological Center (NMC) of China Meteorological Administration

More information

3. As warm, moist air moves into a region, barometric pressure readings in the region will generally 1. decrease 2. increase 3.

3. As warm, moist air moves into a region, barometric pressure readings in the region will generally 1. decrease 2. increase 3. Teacher: Mr. Prizzi Castle Learning Review 1 1. Which process most directly results in cloud formation? 1. condensation 3. precipitation 2. transpiration 4. radiation 2. An air mass originating over north

More information

1., annual precipitation is greater than annual evapotranspiration. a. On the ocean *b. On the continents

1., annual precipitation is greater than annual evapotranspiration. a. On the ocean *b. On the continents CHAPTER 6 HUMIDITY, SATURATION, AND STABILITY MULTIPLE CHOICE QUESTIONS 1., annual precipitation is greater than annual evapotranspiration. a. On the ocean *b. On the continents 2., annual precipitation

More information

Instrumentation planned for MetOp-SG

Instrumentation planned for MetOp-SG Instrumentation planned for MetOp-SG Bill Bell Satellite Radiance Assimilation Group Met Office Crown copyright Met Office Outline Background - the MetOp-SG programme The MetOp-SG instruments Summary Acknowledgements:

More information

Weather Studies Introduction to Atmospheric Science

Weather Studies Introduction to Atmospheric Science Weather Studies Introduction to Atmospheric Science American Meteorological Society Chapter 1 Monitoring The Weather Credit: This presentation was prepared for AMS by Michael Leach, Professor of Geography

More information

Table 1-2. TMY3 data header (line 2) 1-68 Data field name and units (abbreviation or mnemonic)

Table 1-2. TMY3 data header (line 2) 1-68 Data field name and units (abbreviation or mnemonic) 1.4 TMY3 Data Format The format for the TMY3 data is radically different from the TMY and TMY2 data.. The older TMY data sets used columnar or positional formats, presumably as a method of optimizing data

More information

2) What general circulation wind belt is the place of origin for hurricanes? A) westerlies B) trade winds C) doldrums D) horse latitudes

2) What general circulation wind belt is the place of origin for hurricanes? A) westerlies B) trade winds C) doldrums D) horse latitudes Meteo 1010 Homework 6 1) What is the difference between a typhoon and a hurricane? A) A hurricane is a true tropical cyclone, but a typhoon is not. B) A hurricane is stronger than a typhoon. C) They represent

More information

Air Mass Thunderstorms. Air Mass Thunderstorms. Air Mass Thunderstorms. Lecture 26 Air Mass Thunderstorms and Lightning

Air Mass Thunderstorms. Air Mass Thunderstorms. Air Mass Thunderstorms. Lecture 26 Air Mass Thunderstorms and Lightning Lecture 26 and Lightning Life Cycle Environment Climatology Lightning 1 2 Short-lived, isolated thunderstorms that are not severe are often called air-mass thunderstorms. There are three stages describing

More information

Objectives. Vocabulary

Objectives. Vocabulary The Causes of Weather Objectives Compare and contrast weather and climate. Analyze how imbalances in the heating of Earth s surface create weather. Describe how and where air masses form. Vocabulary meteorology

More information

Interpretation of Polar-orbiting Satellite Observations. Atmospheric Instrumentation

Interpretation of Polar-orbiting Satellite Observations. Atmospheric Instrumentation Interpretation of Polar-orbiting Satellite Observations Outline Polar-Orbiting Observations: Review of Polar-Orbiting Satellite Systems Overview of Currently Active Satellites / Sensors Overview of Sensor

More information

Himawari-8 True Color RGB

Himawari-8 True Color RGB Himawari-8 True Color RGB Meteorological Satellite Center, JMA Ver. 20150519 What s True Color RGB? R : B03(VS 0.64) G : B02(V2 0.51) 2015-03-17 00UTC B : B01(V1 0.46) Components of True Color RGB Channel

More information

Average Weather In March For Fukuoka, Japan

Average Weather In March For Fukuoka, Japan Average Weather In March For Fukuoka, Japan Location This report describes the typical weather at the Fukuoka Airport (Fukuoka, Japan) weather station over the course of an average March. It is based on

More information

Dr. Christopher M. Godfrey University of North Carolina at Asheville

Dr. Christopher M. Godfrey University of North Carolina at Asheville Surface and Upper-Air Observations Surface Observations Collect information for synoptic-scale weather Most surface observations are automated (e.g., Automated Surface Observing System) Also mesoscale

More information

Clever Catch Weather Ball Question and Answer Sheets

Clever Catch Weather Ball Question and Answer Sheets Clever Catch Weather Ball Question and Answer Sheets 1. Too much exposure to can cause skin cancer. B. Ultraviolet radiation 2. The layer of the atmosphere closest to the Earth s surface is the 3. Some

More information

Day Microphysics RGB Nephanalysis in daytime. Meteorological Satellite Center, JMA

Day Microphysics RGB Nephanalysis in daytime. Meteorological Satellite Center, JMA Day Microphysics RGB Nephanalysis in daytime Meteorological Satellite Center, JMA What s Day Microphysics RGB? R : B04 (N1 0.86) Range : 0~100 [%] Gamma : 1.0 G : B07(I4 3.9) (Solar component) Range :

More information

Earth Science Lesson Plan Quarter 2, Week 4, Day 1

Earth Science Lesson Plan Quarter 2, Week 4, Day 1 Earth Science Lesson Plan Quarter 2, Week 4, Day 1 1 Outcomes for Today PREPARE 1. Background knowledge necessary for today s reading. In order to make forecasts, meteorologists must gather accurate weather

More information