QUESTION 1 Use the following schematics to explain the local time rate of change of temperature at point A and B as time evolves from the left schematic to the right schematic (qualitatively not quantitatively). Assume that the Lagrangian derivative is zero. The solid lines are isobars at sea level (hPa) and the dashed lines are isotherms (K). Assume that this is in the northern hemisphere and that points A and B are at fixed locations. 1008 hPa 268 1008 a 1004 hPa 1012 270 996 hPa 270 272 274 278 280 278
QUESTION 1 Use the following schematics to explain the local time rate of change of temperature at point A and B as time evolves from the left schematic to the right schematic (qualitatively not quantitatively). Assume that the Lagrangian derivative is zero. The solid lines are isobars at sea level (hPa) and the dashed lines are isotherms (K). Assume that this is in the northern hemisphere and that points A and B are at fixed locations. 1008 hPa 268 1008 a 1004 hPa 1012 270 996 hPa 270 272 274 278 280 278
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
Problem 1LR
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![QUESTION 1
Use the following schematics to explain the local time rate of change of temperature at point A and B as time evolves from the left schematic to the right
schematic (qualitatively not quantitatively). Assume that the Lagrangian derivative is zero. The solid lines are isobars at sea level (hPa) and the dashed lines are
isotherms (K). Assume that this is in the northern hemisphere and that points A and B are at fixed locations.
1008 hPa
268
100s ha
1004 hPa
1012
270
996 hPa
270
272
274
278
274
276
280
278](/v2/_next/image?url=https%3A%2F%2Fcontent.bartleby.com%2Fqna-images%2Fquestion%2F24a60763-065d-4deb-b582-ca07220062f2%2F877a81db-ea43-4437-8552-c61d32c2fe4a%2Fplqb7r_processed.png&w=3840&q=75)
Transcribed Image Text:QUESTION 1
Use the following schematics to explain the local time rate of change of temperature at point A and B as time evolves from the left schematic to the right
schematic (qualitatively not quantitatively). Assume that the Lagrangian derivative is zero. The solid lines are isobars at sea level (hPa) and the dashed lines are
isotherms (K). Assume that this is in the northern hemisphere and that points A and B are at fixed locations.
1008 hPa
268
100s ha
1004 hPa
1012
270
996 hPa
270
272
274
278
274
276
280
278
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