Chapter 3 Weather Maps Surface Station Model
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English Maths
Summer Term Curriculum Overview for Year 5 2021 only Black-First half (The Lion, the Witch and the Wardrobe) Red- Second half (The Secret Garden) English Reading Comprehension Planning, Composing and Evaluating Maths Develop ideas through reading and research Grammar, Punctuation and Vocabulary Use a wide knowledge of text types, forms and styles to inform Check that the text makes sense to them and Fractions B (calculating) (4 weeks) Decimals and percentages (3 weeks) Decimals (5 weeks) their writing Use correct grammatical terminology when discuss their understanding discussing their writing Plan and write for a clear purpose and audience Use imagination and empathy to explore a text Ensure that the content and style of writing accurately reflects Decimals (5 weeks) Geometry: angles (just shape work, angles have been covered) Geometry: position and Use the suffixes –ate, -ise, and –ify to convert nouns beyond the page the purpose or adjectives into verbs Answer questions drawing on information from Borrow and adapt writers’ techniques from book, screen and direction Measurement: volume and converting units Understand what parenthesis is several places in the text stage Recognise and identify brackets and dashes Predict what may happen using stated and Balance narrative writing between action, description and dialogue Use brackets, dashes or commas for parenthesis implied details and a wider personal Geography Evaluate the work of others and suggest improvements Ensure correct subject verb agreement understanding of the world Evaluate their work effectively and make improvements based Name, locate and describe major world cities. Revisit: Identify the location and explain the Summarise using an appropriate amount of detail on this function of the Prime (or Greenwich) Meridian and different time zones (including day and History as evidence Proof–read for spelling and punctuation errors night). -
Years 3–4, and the Others in Years 5–6
Unit 16 What’s in the news? ABOUT THE UNIT This is a ‘continuous’ unit, designed to be developed at various points through the key stage. It shows how news items at a widening range of scales can be used to develop geographical skills and ideas. The unit can be used flexibly when relevant news events occur. The teaching ideas could be selected and used outside designated geography curriculum time, eg during assembly, a short activity at the beginning or end of the day, or within a context for literacy and mathematics work. Alternatively the ideas could be integrated within other geography units where appropriate, eg weather reports could be linked to work on weather and distant localities, see Unit 7. The first three sections are designed to be used in years 3–4, and the others in years 5–6. The unit offers links to literacy, mathematics, speaking and listening and IT. Widening range of scales Undertake fieldwork Wider context Use globes, maps School locality and atlases UK locality Use secondary sources Overseas locality Identify places on Physical and human features maps A, B and C Similarities and differences Use ICT Changes Weather: seasons, world weather Environment: impact Other aspects of skills, places and themes may be covered depending on the content of the news item. VOCABULARY RESOURCES In this unit, children are likely to use: • newspapers • news, current affairs, issues, weather, weather symbols, climate, country, • access to the internet continent, land use, environmental quality, community, physical features, human • local -
General Rules for Contour Lines
6/30/2015 EASC111LabEFor Printing LAB E: Topographic Maps (for printing) MAP READING PRELAB: Any type of map is a twodimensional (flat) representation of Earth’s surface. Road maps, surveying maps, topographic maps, geologic maps can all cover the same territory but highlight different features of the area. Consider the following images from the same area in Illinois. Make a list of the types of features that are shown on each type of map. Topographic Maps The light brown lines on the topographic map are called contour lines. A contour line connects points of equal height above sea level, called elevation. For example, a 600’ (six hundred foot) contour line on a map means that every point on that contour line is 600’ above sea level. In order to understand contour lines better, imagine a box with a “mountain” in it with a clear plastic lid on top of the box. Assume the base of the mountain is at sea level. The box is slowly being filled with water. Since water automatically levels itself off, it will touch the “mountain” at the same height all the way around. If we were to peer down into the box from above, we could draw a line on the lid that marks where the water touches the “mountain”. This would be a contour line for that elevation. As the box continues to fill with water, we would draw contour lines at specific intervals, such as 1”. Each time the water level rises one inch, we will draw a line marking where the water touches the land. -
Maps and Charts
Name:______________________________________ Maps and Charts Lab He had bought a large map representing the sea, without the least vestige of land And the crew were much pleased when they found it to be, a map they could all understand - Lewis Carroll, The Hunting of the Snark Map Projections: All maps and charts produce some degree of distortion when transferring the Earth's spherical surface to a flat piece of paper or computer screen. The ways that we deal with this distortion give us various types of map projections. Depending on the type of projection used, there may be distortion of distance, direction, shape and/or area. One type of projection may distort distances but correctly maintain directions, whereas another type may distort shape but maintain correct area. The type of information we need from a map determines which type of projection we might use. Below are two common projections among the many that exist. Can you tell what sort of distortion occurs with each projection? 1 Map Locations The latitude-longitude system is the standard system that we use to locate places on the Earth’s surface. The system uses a grid of intersecting east-west (latitude) and north-south (longitude) lines. Any point on Earth can be identified by the intersection of a line of latitude and a line of longitude. Lines of latitude: • also called “parallels” • equator = 0° latitude • increase N and S of the equator • range 0° to 90°N or 90°S Lines of longitude: • also called “meridians” • Prime Meridian = 0° longitude • increase E and W of the P.M. -
Print Key. (Pdf)
Weather Map Symbols Along the center, the cloud types are indicated. The top symbol is the high-level cloud type followed by the At the upper right is the In the upper left, the temperature mid-level cloud type. The lowest symbol represents low-level cloud over a number which tells the height of atmospheric pressure reduced to is plotted in Fahrenheit. In this the base of that cloud (in hundreds of feet) In this example, the high level cloud is Cirrus, the mid-level mean sea level in millibars (mb) A example, the temperature is 77°F. B C C to the nearest tenth with the cloud is Altocumulus and the low-level clouds is a cumulonimbus with a base height of 2000 feet. leading 9 or 10 omitted. In this case the pressure would be 999.8 mb. If the pressure was On the second row, the far-left Ci Dense Ci Ci 3 Dense Ci Cs below Cs above Overcast Cs not Cc plotted as 024 it would be 1002.4 number is the visibility in miles. In from Cb invading 45° 45°; not Cs ovcercast; not this example, the visibility is sky overcast increasing mb. When trying to determine D whether to add a 9 or 10 use the five miles. number that will give you a value closest to 1000 mb. 2 As Dense As Ac; semi- Ac Standing Ac invading Ac from Cu Ac with Ac Ac of The number at the lower left is the a/o Ns transparent Lenticularis sky As / Ns congestus chaotic sky Next to the visibility is the present dew point temperature. -
Eye-Tracking Evaluation of Weather Web Maps
International Journal of Geo-Information Article Eye-tracking Evaluation of Weather Web Maps Stanislav Popelka , Alena Vondrakova * and Petra Hujnakova Department of Geoinformatics, Faculty of Science, Palacký University Olomouc, 17. listopadu 50, 77146 Olomouc, Czech Republic; [email protected] (S.P.); [email protected] (P.H.) * Correspondence: [email protected]; Tel.: +420585634517 Received: 30 November 2018; Accepted: 28 May 2019; Published: 30 May 2019 Abstract: Weather is one of the things that interest almost everyone. Weather maps are therefore widely used and many users use them in everyday life. To identify the potential usability problems of weather web maps, the presented research was conducted. Five weather maps were selected for an eye-tracking experiment based on the results of an online questionnaire: DarkSky, In-Poˇcasí, Windy, YR.no, and Wundermap. The experiment was conducted with 34 respondents and consisted of introductory, dynamic, and static sections. A qualitative and quantitative analysis of recorded data was performed together with a think-aloud protocol. The main part of the paper describes the results of the eye-tracking experiment and the implemented research, which identify the strengths and weaknesses of the evaluated weather web maps and point out the differences between strategies in using maps by the respondents. The results include findings such as the following: users worked with web maps in the simplest form and they did not look for hidden functions in the menu or attempt to find any advanced functionality; if expandable control panels were available, the respondents only looked at them after they had examined other elements; map interactivity was not an obstacle unless it contained too much information or options to choose from; searching was quicker in static menus that respondents did not have to switch on or off; the graphic design significantly influenced respondents and their work with the web maps. -
Weather Forecasting Activities.Pdf
Weather Forecasting Weather Map and Forecasting Practice Incorporating a Fusion of Knowledge Involving Air Masses, Fronts, and Air Pressure Content Weather Forecasting Below, match the map with the appropriate profession: Weather Map Meteorologist Use the symbols below as a reference: Cold Front Warm Front High Pressure Low Pressure Clouds Rain Thunderstorms Hurricane Weather Conditions City Sunny, high temperature of 82°F Thunderstorms, high temperature of 91°F Sunny, high temperature of 75°F Rain, high temperature of 80°F Partly cloudy, high temperature of 73°F Mostly cloudy, high temperature of 92°F Scenario Answer Showers and thunderstorms; HOT and humid Hurricane just off the coast Center of low pressure Cold front Cool with highs in the low 70’s Sunny and VERY HOT!!! Color Precipitation Type Image SNOW RAIN ICE Detroit, Michigan Boston, Massachusetts Philadelphia, Pennsylvania Raleigh, North Carolina Phoenix, Arizona Orlando, Florida Weather Conditions City Moderate/Heavy Snow Warm and Dry Showers and Thunderstorms Ice Cold and Dry Minneapolis Houston San Francisco New York City Seattle Atlanta Miami Texas Between Chicago and Wyoming New York City Southern California and Seattle Arizona Philadelphia Raleigh Orlando Boston/Detroit Phoenix 3 Day Weather Forecasting Weather Map and Forecasting Practice Incorporating a Fusion of Knowledge Involving Atmospheric Variables Philadelphia,, PA Madison, WI Pittsburgh,PA Chicago, IL Flagstaff, AZ Atlanta, GA Phoenix, AZ The above is a daily weatha er map for which date? a DECEMBER 24, 2013 MAY 14, 2014 On the weather map above the forecasted weather is: A VARIETY SIMILAR Weather Forecast for Wednesday May 14, 2014 City Weather Forecast Image Atlanta, GA Pittsburgh, PA Madison, WI Phoenix, AZ Flagstaff, AZ Use the following information to make a reasonable weather forecast for the next day: Thursday May 15, 2014 Over the course of the next 24 hours the low pressure system in Louisiana will track to the northeast along the cold front . -
9 Weather Reports & Map Analysis
Copyright © 2017 by Roland Stull. Practical Meteorology: An Algebra-based Survey of Atmospheric Science. v1.02b 9 WEATHER REPORTS & MAP ANALYSIS Contents Surface weather charts summarize weather con- ditions that can affect your life. Where is it raining, 9.1. Sea-level Pressure Reduction 267 snowing, windy, hot or humid? More than just plots 9.2. Meteorological Reports & Observations 268 of raw weather reports, you can analyze maps to 9.2.1. Weather Codes 268 highlight key features including airmasses, centers 9.2.2. METAR and SPECI 270 of low- and high-pressure, and fronts (Fig. 9.1). In 9.2.3. Weather-Observation Locations 271 this chapter you will learn how to interpret weather 9.3. Synoptic Weather Maps 274 reports, and how to analyze surface weather maps. 9.3.1. Station Plot Model 274 9.3.2. Map Analysis, Plotting & Isoplething 280 9.4. Review 282 9.5. Homework Exercises 282 9.1. SEA-LEVEL PRESSURE REDUCTION 9.5.1. Broaden Knowledge & Comprehension 282 9.5.2. Apply 282 Near the bottom of the troposphere, pressure 9.5.3. Evaluate & Analyze 287 9.5.4. Synthesize 287 gradients are large in the vertical (order of 10 kPa km–1) but small in the horizontal (order of 0.001 kPa km–1). As a result, pressure differences between neighboring surface weather stations are dominated by their relative station elevations zstn (m) above sea level. However, horizontal pressure variations are im- cP portant for weather forecasting, because they drive H horizontal winds. To remove the dominating influ- ence of station elevation via the vertical pressure gradient, the reported station pressure Pstn is extrap- L olated to a constant altitude such as mean sea level (MSL). -
Topographic Maps Fields
Topographic Maps Fields • Field - any region of space that has some measurable value at every point. • Ex: temperature, air pressure, elevation, wind speed Isolines • Isolines- lines on a map that connect points of equal field value • Isotherms- lines of equal temperature • Isobars- lines of equal air pressure • Contour lines- lines of equal elevation Draw the isolines! (connect points of equal values) Isolines Drawn in Red Isotherm Map Isobar Map Topographic Maps • Topographic map (contour map)- shows the elevation field using contour lines • Elevation - the vertical height above & below sea level Why use sea level as a reference point? Topographic Maps Reading Contour lines Contour interval- the difference in elevation between consecutive contour lines Subtract the difference in value of two nearby contour lines and divide by the number of spaces between the contour lines Elevation – Elevation # spaces between 800- 700 =?? 5 Contour Interval = ??? Rules of Contour Lines • Never intersect, branch or cross • Always close on themselves (making circle) or go off the edge of the map • When crossing a stream, form V’s that point uphill (opposite to water flow) • Concentric circles mean the elevation is increasing toward the top of a hill, unless there are hachures showing a depression • Index contour- thicker, bolder contour lines on contour maps, usually every 5 th line • Benchmark - BMX or X shows where a metal marker is in the ground and labeled with an exact elevation ‘Hills’ & ‘Holes’ A depression on a contour map is shown by contour lines with small marks pointing toward the lowest point of the depression. The first contour line with the depression marks (hachures) and the contour line outside it have the same elevation. -
Weather Forecasting Webquest
Weather Forecasting Webquest Name ____________________________________________________________ Begin by going to the following website: http://www.oar.noaa.gov/k12/html/forecasting2.html Click on the Get info.1 link Weather Symbols Click on the symbols site…. Read the chart and fill in the symbols. Click "Back" to return to the Forecasting "Get Info.1" web page. Cloud Cover Symbols Click on the "Project Cloud Cover" site. 1. Describe how you would show that the sky was 50% cloudy. 2. Draw a sky that has about 10% cloud coverage Click back and then…… Storm Structure Click on the "Project Wind Speed Symbols" site 1. How do you show the direction the wind is blowing from? 2. What is the relationship between the length of the lines on the barb and the wind speed? 3. Draw a picture that would represent southernly wind blowing about 15 knots with clear skies. 4. Draw a model that would show a northwesterly wind blowing at 20 knots with 25% cloud cover. 5. Convert 20 knots to miles per hour (show how you got your answer). 6. Draw a station model (wind barb) showing 86 miles per hour southwesterly wind and completely overcast skies (first convert to knots from mph) Click back to return to “Get Info.1” then foreward at bottom of page Isobars Click on the Project Isobars site. 1. What are isobars? 2. Describe how the wind would move at a: Cyclone – Anti-cyclone – 3. Using what you just read about, how can we use isobars to show the direction that the wind is blowing? Click back and then to the “Get info.2” web page, then the Weather Systems page 1. -
Lecture 14. Extratropical Cyclones • in Mid-Latitudes, Much of Our Weather
Lecture 14. Extratropical Cyclones • In mid-latitudes, much of our weather is associated with a particular kind of storm, the extratropical cyclone Cyclone: circulation around low pressure center Some midwesterners call tornadoes cyclones Tropical cyclone = hurricane • Extratropical cyclones derive their energy from horizontal temperature con- trasts. • They typically form on a boundary between a warm and a cold air mass associated with an upper tropospheric jet stream • Their circulations affect the entire troposphere over a region 1000 km or more across. • Extratropical cyclones tend to develop with a particular lifecycle . • The low pressure center moves roughly with the speed of the 500 mb wind above it. • An extratropical cyclone tends to focus the temperature contrasts into ‘fron- tal zones’ of particularly rapid horizontal temperature change. The Norwegian Cyclone Model In 1922, well before routine upper air observations began, Bjerknes and Sol- berg in Bergen, Norway, codified experience from analyzing surface weather maps over Europe into the Norwegian Cyclone Model, a conceptual picture of the evolution of an ET cyclone and associated frontal zones at ground They noted that the strongest temperature gradients usually occur at the warm edge of the frontal zone, which they called the front. They classified fronts into four types, each with its own symbol: Cold front - Cold air advancing into warm air Warm front - Warm air advancing into cold air Stationary front - Neither airmass advances Occluded front - Looks like a cold front -
Gradual Generalization of Nautical Chart Contours with a B-Spline Snake Method
GRADUAL GENERALIZATION OF NAUTICAL CHART CONTOURS WITH A B-SPLINE SNAKE METHOD BY DANDAN MIAO BS in Geographic Information Systems, Wuhan University, 2009 THESIS Submitted to the University of New Hampshire in Partial Fulfillment of the Requirements for the Degree of Master of Science in Ocean Engineering September, 2014 ALL RIGHTS RESERVED © 2014 Dandan Miao This thesis has been examined and approved. Dr. Brian Calder, Associate Research Professor of Ocean Engineering Dr. Kurt Schwehr Affiliate Associate Professor of Ocean Engineering Dr. Steve Wineberg Lecturer, Mathematics and Statistics Date v ACKNOWLEDGMENTS This study was sponsored by NOAA grant NA10NOS400007, and supported by the Center for Coastal and Ocean Mapping. Professor Larry Mayer introduced me to the world of Ocean Mapping, and taught me new information about geological oceanography; Professor Brian Calder initiated this study and has always been able to selflessly help me with any questions; Professor Steven Wineberg gave me many insights of how to transfer math concepts to graphic behavior; Professor Kurt Schwehr helped me with many intelligent thoughts and suggestion about computer programming implementation. I am grateful for all their selfless help and patience, and I would like to thank all of them for their guidance, encouragement and proof-reading of this thesis: without them and CCOM’s support, this work would not have happened. Finally, I would like to thank my parents and friends, for encouragement and trust. Your love and faith gave me the strength to keep holding on and finally make it work! Love you all! With greatest thankfulness, Dandan Miao vi TABLE OF CONTENTS ACKNOWLEDGMENTS .............................................................................................................