Tracking Typhoons PDF
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UiTM Cawangan Pulau Pinang Kampus Bertam
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Summary
This document provides an overview of typhoon tracking and forecasting, the effects of landforms and bodies of water on typhoon development, and how to analyze rainfall advisory systems relating to typhoons.
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Welcome to the world of science Tracking of Typhoons ▸ Be familiar with rainfall advisory ▸ Explain the effect of mountains and bodies of water on typhoon development ▸ Trace the pathway of typhoon that enters the Philippine Area of Responsibility (PAR) using a map and tracking data....
Welcome to the world of science Tracking of Typhoons ▸ Be familiar with rainfall advisory ▸ Explain the effect of mountains and bodies of water on typhoon development ▸ Trace the pathway of typhoon that enters the Philippine Area of Responsibility (PAR) using a map and tracking data. 2 Tracking of typhoons Name that rainfall advisory 4 Name that rainfall advisory 5 6 How landforms and bodies of water affect typhoons Effect of landforms Orographic Orography- precipitation- study of the rain, snow, or formation other precipitation and produced when moist air is lifted topography of as it moves over a mountains mountain range. and hills 9 Effect of landforms Orography- study of the Orography- formation study of the and formation topography of and mountains topography of and hills mountains and hills 10 Effects of Bodies of Water Ingredients of Typhoon Formation ▸ abundant warm water ▸ high humidity ▸ optimal location ▸ ocean water (26.50C) ▸ spanning from the surface up to the depth of at least 50 meters ▸ low vertical wind shear 11 Effects of Bodies of Water Bodies of Water- determine whether the air temperature will be warm or cold, or if the relative humidity will be high or low. 12 Name that Process! Landform e. Air cools as it continues to rise f. Humidity condenses into heavy rain g. Warm, humid air travels into the land Bodies of Water a. Humid air is rising making the clouds b. Winds flow outward above the storm, allowing the air blow to rise c. Light winds outside typhoon steer it and let it grow d. Winds coming together forcing air upward 13 Name that Process! f. Humidity condenses b. Winds flow outward into heavy rain above the storm, allowing the air e. Air cools as it below to rise continues to rise c. Light winds outside a. Humidity air is rising typhoon steer it and making the clouds of let it grow the storm g. Warm, humid air d. Winds coming travels into the land together forcing air upward 14 Tracking of a typhoon What do you call that image you see below? Philippine Area of Responsibility *(PAR) “ 16 Tracking of a typhoon ▸Typhoon tracking and forecasting involve the prediction of the path of a typhoon every 6 to 12 hours over a period of at least five days. ▸With this, PAGASA uses a variety of meteorological tools and methods to deliver accurate forecasts. ▸The weather in a specific location will show signs of an approaching typhoon, like an increasing wave height and frequency, increasing cloudiness, falling air pressure, and heavy rainfall. 17 Tracking of a typhoon ▸Accurate track prediction depends in the position and strength of high- and low-pressure areas, and on how those areas will migrate during the lifetime of a tropical system. ▸Computer forecast models aid in determining this motion at least 5 to 7 days ahead. ▸An accurate track forecast is essential because if the track forecast goes wrong, the intensity, rainfall, storm surge, and tornado threat will also be incorrect. 18 Tracking of a typhoon ▸Accurate track prediction depends in the position and strength of high- and low-pressure areas, and on how those areas will migrate during the lifetime of a tropical system. ▸Computer forecast models aid in determining this motion at least 5 to 7 days ahead. ▸An accurate track forecast is essential because if the track forecast goes wrong, the intensity, rainfall, storm surge, and tornado threat will also be incorrect. Weather Surveillance Radar 19 Dissecting a Typhoon 20 Dissecting a Typhoon ▸Location A is the eyewall of the typhoon. B, C, and D are locations that are getting farther from the eye. The air pressures at the different locations are: 21 Dissecting a Typhoon ▸Location E is within the eye of the typhoon. Location F is within the clouds surrounding the eye. The clouds at F make up the eyewall. The wind speeds at the two locations are: 22 Tracking of a typhoon ▸Accurate track 23 Tracking of a typhoon ▸Accurate track 24 Tracking of a typhoon ▸Accurate track 25 Tracking of a typhoon ▸Accurate track 26 Tracking of a typhoon ▸Accurate track 27 Tracking of a typhoon ▸Accurate track 28 Tracking of a typhoon ▸Accurate track 29 Tracking of a typhoon Tropical Storm (TS) wind speed: 66 t0 88 kph 30 Answer me! ▸Where did tropical storm Sendong start to form? Pacific ocean 31 Answer me! ▸Where did tropical storm Sendong start to form? Pacific ocean 32 Answer me! ▸Where did tropical storm Sendong enter PAR? 12/15/2011 12:00 AM 33 Answer me! ▸When did tropical storm Sendong leave PAR? 12/18/2011 12:00 PM 34 Answer me! ▸In What direction did tropical storm Sendong move? Northwest 35 Answer me! ▸In What direction did tropical storm Sendong move? Northwest 36 Thank you for Listening! Thank You for Listening! 37 38