PPT-The De-correlation of Westerly Winds and Westerly-Wind Stre
Author : marina-yarberry | Published Date : 2016-08-11
Objective Reconcile the conflicting evidence of the meridional westerly wind shift during the Last Glacial Maximum LGM indicated by proxyrecords from the atmosphere
Presentation Embed Code
Download Presentation
Download Presentation The PPT/PDF document "The De-correlation of Westerly Winds and..." is the property of its rightful owner. Permission is granted to download and print the materials on this website for personal, non-commercial use only, and to display it on your personal computer provided you do not modify the materials and that you retain all copyright notices contained in the materials. By downloading content from our website, you accept the terms of this agreement.
The De-correlation of Westerly Winds and Westerly-Wind Stre: Transcript
Objective Reconcile the conflicting evidence of the meridional westerly wind shift during the Last Glacial Maximum LGM indicated by proxyrecords from the atmosphere and ocean Approach. This particular trial is testing 57479 The use of performance based navigation PBN 57521 PBN moves aviation away from the traditional use of aircraft navigating by ground based beacons to a system more reliant on airborne technologies utilising Area Coriolis. Effect. Air pressure differences cause the movement of air. Air moving parallel to the ground is called . wind. Air moving up or down is called a . current. Air generally moves from the poles to the equator, . Simple things to watch for and assist you in getting better . scores. By Rob Rush. The Perfect Shot. The flight path of a projectile is influenced by a number of factors such as;. Bullet shape ( Ballistic Coefficient). G. VanNada. What are they?. Tropical cyclones that cross the subtropical ridge axis into the Westerlies recurve due to increased westerly flow. The winds are predominantly from the southwest in the Northern Hemisphere and from the northwest in the Southern Hemisphere. Why Air Moves. Wind is created by differences in air pressure. Bigger difference = faster wind. Caused by unequal heating of earth. Air. The air by the equator is warm and rises. Low pressure. The air by the poles is cold and dense. Chapter 2.2 Guided Notes. What is Weather?. Weather is the condition of Earth’s atmosphere at a particular time and place.. What is Wind. ?. Wind is air moving across the surface of the Earth. It can move horizontally or parallel to the ground.. The movement of air in a horizontal direction. What is wind?. The uneven heating of the Earth causes differences in air pressure.. What causes wind?. The Sun’s energy is more concentrated at the Equator and spread out more over the poles.. The movement of air in a horizontal direction. What is wind?. The uneven heating of the Earth causes differences in air pressure.. What causes wind?. The Sun’s energy is more concentrated at the Equator and spread out more over the poles.. Summary of the measure of the characteristics of individuals in groups.. A descriptive statistic talks about a single characteristics within a given group. Lots of descriptive statistics are summarizing lots of characteristics but all within a given group.. What causes wind? . Caused by a difference in air pressure due to. unequal heating of the atmosphere.. Winds are created by. ….. • . Heating the air, decreases pressure (warm. air rises creating a low pressure). Wind is the movement . of air caused by an uneven heating of the Earth’s . surface.. What HEATS EARTH’S SURFACE?. Heat from the sun heats the surface of the Earth.. This heat arrives to Earth in the form of radiation.. John King and Thomas Bracegirdle. British Antarctic Survey. Cambridge, UK. jcki@bas.ac.uk. S. tart presentation. Introduction to the Antarctic coastal . e. asterlies. Climatology of the Antarctic coastal . air. or other gases relative to a earth’s surface. . Global winds resulting from the difference in absorption of solar energy between the climatic zones on earth. . Winds . occur on a range of scales, from thunder storms where flows lasting tens of minutes, to local breezes generated by heating of . Local winds are caused by the movement of air between low-pressure and high-pressure systems within small areas. As there are so many different types of winds, each one takes on a unique form. Local winds frequently have a significant impact on climate in local regions, so it is critical to understand what causes them..
Download Document
Here is the link to download the presentation.
"The De-correlation of Westerly Winds and Westerly-Wind Stre"The content belongs to its owner. You may download and print it for personal use, without modification, and keep all copyright notices. By downloading, you agree to these terms.
Related Documents