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3. The figure below shows maps of pressure distributions in several situations. Keeping in mind the influence of pressure gradient force, Coriolis effect, and surface friction, use arrows to indicate the appropriate resultant wind directions corresponding to the isobaric patterns for geostrophic wind (left column) and surface wind (right column) on maps below GEOSTROPHIC WIND SURFACE WIND 510 High 1012 512 mb High USA 1000 512 Low 1000 510 Low 1012 mb RUSTRALIA

3. The figure below shows maps of pressure distributions in several situations. Keeping in mind the influence of pressure gradient force, Coriolis effect, and surface friction, use arrows to indicate the appropriate resultant wind directions corresponding to the isobaric patterns for geostrophic wind (left column) and surface wind (right column) on maps below GEOSTROPHIC WIND SURFACE WIND 510 High 1012 512 mb High USA 1000 512 Low 1000 510 Low 1012 mb RUSTRALIA

Applications and Investigations in Earth Science (9th Edition)
Applications and Investigations in Earth Science (9th Edition)
9th Edition
ISBN:9780134746241
Author:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Publisher:Edward J. Tarbuck, Frederick K. Lutgens, Dennis G. Tasa
Chapter1: The Study Of Minerals
Section: Chapter Questions
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12:41 80% e 03 Image Тext E Open with Google Docs 3. The figure below shows maps of pressure distributions in several situations. Keeping in mind the influence of pressure gradient force, Coriolis effect, and surface friction, use arrows to indicate the appropriate resultant wind directions corresponding to the isobaric patterns for geostrophic wind (left column) and surface wind (right column) on maps below GEOSTROPHIC WIND SURFACE WIND 510 High 1012 512 mb High 1000 512 Low 1000. 510 Low 1012 mb RUSTRALIA Page 2 7 3/3 Rotate Markup Word Signature Note
Transcribed Image Text:12:41 80% e 03 Image Тext E Open with Google Docs 3. The figure below shows maps of pressure distributions in several situations. Keeping in mind the influence of pressure gradient force, Coriolis effect, and surface friction, use arrows to indicate the appropriate resultant wind directions corresponding to the isobaric patterns for geostrophic wind (left column) and surface wind (right column) on maps below GEOSTROPHIC WIND SURFACE WIND 510 High 1012 512 mb High 1000 512 Low 1000. 510 Low 1012 mb RUSTRALIA Page 2 7 3/3 Rotate Markup Word Signature Note
12:43 80% e 04 Image Тext Drawing Isobars. Practice in drawing isobars (lines of equal pressure) on a weather map and figuring out how surface winds move diagonally across them will increase your ability to read and interpret not only daily weather maps, but also global maps of pressure and winds. The map on the following page shows barometric pressures observed simultaneously at many National Weather Service stations. Pressures at each Jocation are given in millibars (mb), but only the last two digits are given. Thus "10" designates 1010 mb; "96" designates 996, elc. Each statlion is located at the dot alongside the number, 4. On the map on the fo: ng cagel (1; draw ikobaroior th entire map using a 4 mb interval, starting at 992 mb. n other words. draw isdbar lines for values 992, 996, 4/4 Rotate Markup Word Signature Note
Transcribed Image Text:12:43 80% e 04 Image Тext Drawing Isobars. Practice in drawing isobars (lines of equal pressure) on a weather map and figuring out how surface winds move diagonally across them will increase your ability to read and interpret not only daily weather maps, but also global maps of pressure and winds. The map on the following page shows barometric pressures observed simultaneously at many National Weather Service stations. Pressures at each Jocation are given in millibars (mb), but only the last two digits are given. Thus "10" designates 1010 mb; "96" designates 996, elc. Each statlion is located at the dot alongside the number, 4. On the map on the fo: ng cagel (1; draw ikobaroior th entire map using a 4 mb interval, starting at 992 mb. n other words. draw isdbar lines for values 992, 996, 4/4 Rotate Markup Word Signature Note
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