LEADING CADET. Navigation with Map and Compass Navigation is about knowing where you are on the map

Similar documents
Unit: Weather Study Guide

Weather Notes. Chapter 16, 17, & 18

Using Map and Compass Together

Weather is the of the Earth s atmosphere at a place and time. It is the movement of through the atmosphere o Energy comes from the

Earth Science Chapter 16 and 17. Weather and Climate

Warm-Up Draw a picture of the water cycle

Name Class Date. Water molecules condense around the salt crystal. More water molecules condense around the original small droplet.

AIR MASSES. Large bodies of air. SOURCE REGIONS areas where air masses originate

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

BUSH NAV BUSH NAV DAY Navigation for Bush Navigation Day. November. WhitehorseD AY. Section 1 Registration, Maps & Checkpoints

Weather, Air Masses, Fronts and Global Wind Patterns. Meteorology

according to and water. High atmospheric pressure - Cold dry air is other air so it remains close to the earth, giving weather.

Cloud Formation and Classification

Objectives: S.W.B.A.T.

NAVIGATION. 2. Marginal Information

Air Masses and Fronts II

Clouds. How Clouds Form. Humidity. Determining Relative Humidity

Mid-latitude Cyclones & Air Masses

Clouds. What they tell us about the weather

Atmospheric Conditions Geography Notes JC-Learn. JC-Learn. Geography Notes Atmospheric Conditions. 1 P a g e

Unit 4 Lesson 2 Clouds and Cloud Formation. Copyright Houghton Mifflin Harcourt Publishing Company

Weather. Chapter Test A. Multiple Choice. Write the letter of the correct answer on the line at the left.

Mr. P s Science Test!

How our atmosphere is heated.

WATER IN THE ATMOSPHERE

COMPOSITION OF THE ATMOSPHERE

Earth Science final exam study guide (Semester 2)

Condensation is the process by which water vapor changes from a gas to a liquid. Clouds form by this process.

Navigation. A question. Take a map and remove the actual map and what are you left with?

AOSC 200 Tim Canty. Class Web Site: Topics for today: Air Masses. Fronts. Lecture 19 Apr

Pd: Date: Page # Weather Patterns -- Lesson 2 Study Guide

Meteorology Clouds and Fog. Cloud Classification MTPs: Height. Shape. and. Clouds are classified by:

Atmosphere and Weather Revision Notes

November 28, 2017 Day 1

ISSUED BY KENDRIYA VIDYALAYA - DOWNLOADED FROM

777 GROUNDSCHOOL Temperature, Stability, Fronts, & Thunderstorms

Unit 4 Review Guide: Weather

5.04 Clouds and Fog. References: FTGU pages , 147. Meteorology

Global Winds AOSC 200 Tim Canty

Forecasting Weather: Air Masses and Fronts

REVISION: MAPWORK 18 SEPTEMBER 2014

Condensation is the process by which water vapor changes from a gas to a liquid. Clouds form by this process.

Weather Systems. Section

Unit 5 Part 2 Test PPT

Fig Major air masses of the world

Compass Basics. Quick Map Basics Review For Compass Use

Clouds. Naming/Classifying Clouds. Cloud Heights. Height above ground level Shape

ESCI 344 Tropical Meteorology Lesson 7 Temperature, Clouds, and Rain

Air Masses and Fronts

FORMATION OF AIR MASSES

The most abundant gas in the atmosphere by volume is. This gas comprises 78% of the Earth atmosphere by volume.

What does a raindrop look like as it is falling? A B C

Clouds By Patti Hutchison

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

Weather Elements (air masses, fronts & storms)

12/22/2018. Water and the Atmosphere. 8 th Grade. Lesson 1 (Water in the Atmosphere) Chapter 4: Weather. Lesson 2 (Clouds) Clouds

Weather. Weather Patterns

What do you think of when someone says weather?

Air Masses and Fronts. Ahrens Chapter 12

Final Weather Unit Study Guide

20.1 Air Masses. Weather Patterns and Severe Storms. Four Types of Source Regions. Weather in North America Fronts

air masses and Fronts 2013.notebook January 29, 2013

CLIMATE. UNIT TWO March 2019

The Navigator s Dozen

Chapter22 Weather Maps

Name: Period: Air Masses Notes 7 Minutes Page 2 Watch the air masses video. Make sure you follow along.

Chapter 5: Forms of Condensation and Precipitation. Copyright 2013 Pearson Education, Inc.

Red Star Navigation. Bearings:

3 Weather and Climate

Use the terms from the following list to complete the sentences below. Each term may be used only once.

Moisture, Clouds, and Precipitation Earth Science, 13e Chapter 17

Weather Unit Part 2: Meteorology

True or false: The atmosphere is always in hydrostatic balance. A. True B. False

SPI Analyze data to identify events associated with heat convection in the atmosphere. SPI Recognize the connection between the

A. Weather - the conditions of the variables of the atmosphere for any short period of time

ENABLING OBJECTIVE AND TEACHING POINTS. BUSHCRAFT: TIME two 30 minute periods.

Science 1206 Weather Unit REVIEW Short Answer

Polar regions Temperate Regions Tropics High ( cirro ) 3-8 km 5-13 km 6-18 km Middle ( alto ) 2-4 km 2-7 km 2-8 km Low ( strato ) 0-2 km 0-2 km 0-2 km

NATS 1750 Lecture. Wednesday 28 th November Pearson Education, Inc.

Condensation: Dew, Fog, & Clouds. Chapter 5

Meteorology Unit Study Guide

Bell Ringer. 1. What is humidity? 2. What kind of clouds are there outside right now? 3. What happens to air when it gets colder?

Atmosphere L AY E RS O F T H E AT MOSPHERE

Chapter 12 Fronts & Air Masses

Air Masses of North America cp and ca air masses Air mass characterized by very cold and dry conditions

25.1 Air Masses. Section 25.1 Objectives

Chapter 18/19. Ch 18

Atmosphere, Weather & Climate Review for Unit Assessment (Can be taken on Study Island Due Mon., 11/26/12)

Chapter 6. Cloud Development and Forms

WATER IN THE ATMOSPHERE

DEPARTMENT OF GEOSCIENCES SAN FRANCISCO STATE UNIVERSITY. Metr Fall 2012 Test #1 200 pts. Part I. Surface Chart Interpretation.

USING THE MILITARY LENSATIC COMPASS

What a Hurricane Needs to Develop

Meteorology B Station 1 AIR MASSES. Examine this weather map. Please share nicely, as two teams will need to use the map.

Orienteering Maps & Map Reading Latitude and Longitude Scale

9/13/2012. Chapter 4. Atmospheric Moisture, Condensation, and Clouds.

Chapter 4. Atmospheric Moisture, Condensation, and Clouds. 9/13/2012

Seasons, Global Wind and Climate Study Guide

Earth Science. Lab 21: Weather Patterns

6.2 Meteorology. A meteorologist is a person who uses scientific principles to explain, understand, observe, or forecast Earth s weather.

Transcription:

LEADING CADET Navigation with Map and Compass Navigation is about knowing where you are on the map Revision Notes Learning Outcome 1 Be able to find a position with an Ordnance Survey map using the physical features of the land Two Methods of finding North without a Compass (LEARN) Remember using a watch gives the SOUTH direction initially When using a map the first action is to set or orientate it by positioning it relative to features on the ground Learning Outcome 2 Know the different types of north Remember the following symbols Magnetic North in the UK differs from both True North and Grid North The difference between True North and Grid North arises because the lines of latitude and longitude do not match the grid lines exactly TRUE MAGNETIC GRID The position of the Magnetic North pole changes every year The Magnetic Pole is currently located to the north of Hudson Bay in Canada When navigating with a map Grid North is always used for reference 1

Magnetic Variation is the angular difference between True North and Magnetic North and on an OS map information on the Magnetic Variation is located at the bottom right hand side Grid Magnetic Angle (GMA) is the angular difference between Grid North and Magnetic North and on an OS map information the GMA is located at the centre of the top margin Convergence is the approximate difference between True North and Grid North and is between 0 and 5 degrees but not more than 2 degrees in most places. It occurs because the converging lines of longitude do not exactly match the parallel grid lines Lines of Longitude get closer together as they approach the North Pole. Finding the Pole Star by using the Plough star group enables North to be located at night Grid lines on a map point to Grid North Learning Outcome 3 Be able to use a lightweight compass for practical navigation When navigating with a compass we are making use of the Earth s magnetic field A freely suspended magnet will point to the Magnetic North pole A Silva compass is used for navigating when walking On a Silva compass the magnetic needle is red and white. The scale used on the compass is in millimetres The purpose of the liquid in the compass capsule is to allow the needle to move freely then settle down quickly to steady it to take a reading The compass should be held horizontal when reading to allow the needle to swing freely Magnetic Deviation is the effect on the compass needle of nearby ferrous objects or computer screens A Grid bearing is converted to a Magnetic bearing by adding the GMA (GRID to MAG ADD) A Magnetic bearing is converted to a Grid bearing by subtracting the GMA (MAG to GRID GET RID) When setting a map with a compass the first step is to set the GMA against the compass index mark The final step in setting a map with a compass is to turn the map and compass together until the needle is inside the orientating arrow To take a bearing on a distant object you first point the compass direction of travel arrow at the object To take a bearing between 2 features on a map you first place the compass on the map so its longest edge runs through both features you then turn the compass capsule until the orientating lines are parallel with the north-south grid lines When walking on a bearing in good visibility the best technique is to select a distant feature that is along your intended route and walk towards it 2

Resection means fixing your position on a map using three prominent landmarks. The landmark bearings are taken with a compass. These bearings are then plotted on a map and your position is in the middle of the triangle formed by the three intersecting plot lines The best way to measure distances on a map without a pair of dividers is to use the straight edge of a piece of paper and mark it with a pencil Learning Outcome 4 Know land navigation methods Measuring distances accurately helps you to keep on schedule and to reduce the uncertainty of your position The best way to measure distances on a map without a pair of dividers is to use the straight edge of a piece of paper and mark it with a pencil Handrailing is following linear features to get to your destination Countouring means walking around a hill without gaining or losing height An attack point is an easily identifiable feature that is close to your objective The estimated speed of a group on level ground is 4kph To estimate distance covered from last check point - measure the time taken and calculate at 4km/hr Distance from your last check point can be estimated by measuring the time taken and calculate at 4kph Pacing should only be used over short distances Naismith s Rule applies to speed of advance in mountainous terrain (steep terrain) when under such conditions: 20 minutes should be added for every 200 metres ascended in a journey (1min per 10m) 10 minutes should be added for every 200 metres descended in a journey A Roamer is used to read grid references and ensures better accuracy A 4 figure grid reference refers to the SW corner of the grid square 3

Learning Outcome 5 Be able to recognise weather conditions that affect land navigation The relationship of the Upper and Lower winds can be used to indicate the weather shortly to reach you Weather Fronts 1 Cold 2 Warm 3 Stationary 4 Occluded Fronts occur when a cold air mass meets a warm air mass A Depression is an area of Low Pressure; it moves under the influence of Upper winds An Anticyclone is an area of High Pressure; it tends to bring long periods of fine weather An Occluded Front occurs when a cold air mass meets a warm air mass Isobars join points of equal atmospheric pressure Air Masses W Polar Maritime (brings cool winds and heavy showers to the UK in both summer and winter) X Tropical Maritime (originates around the equator and brings warm, cloudy weather to the UK in both summer and winter)* Y Artic Maritime Z- Tropical Continental (Hot and very dry, originating from the arid and desert regions during summer. Can bring record heat to the UK, particularly in late-summer. W - Returning Polar Maritime (mass starts off very cold with dry air but arrives in the UK warm and wet) In addition, the Polar continental air mass via the short seatrack (not shown on diagram) brings cold dry weather with little or no cloud to the British Isles in winter* Remember in particular 4

Cloud Types and Formations Cloud Type Prefix Height Cirrus, Cirrostratus, Cirrocumulus Alto, Altocumulus Nimbostratus Stratocumulus, Cumulus Cirro Alto Nimbo Strato High Medium Medium/Low Low Remember CANS for descending cloud types Low Level Medium Level High Level Cumulus Altocumulus Cirrocumulus Stratus Cirrus Remember that Stratus clouds occur as a featureless layer 5