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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 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)
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
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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