We have spent some time discussing reactions that occur in aqueous media and devoted some attention to the properties of water that make it unique. Now consider the power required to drive the hydrologic cycle, assuming that annual global rainfall averages 1 m across the approximately 5.1 ´ 1014 m2 of earth’s surface. What is the energy required to drive the hydrologic cycle? How does this compare with incoming solar radiation and world energy consumption? Consider the following data: Latent heat of vaporization = 2465 kJ/kg for water at 15⁰C. In 1987 world energy consumption was estimated at 3.3 ´ 1017 kJ Incoming sunlight absorbed at 168 W/m2 at earth’s surface
We have spent some time discussing reactions that occur in aqueous media and devoted some attention to the properties of water that make it unique. Now consider the power required to drive the hydrologic cycle, assuming that annual global rainfall averages 1 m across the approximately 5.1 ´ 1014 m2 of earth’s surface. What is the energy required to drive the hydrologic cycle? How does this compare with incoming solar radiation and world energy consumption? Consider the following data: Latent heat of vaporization = 2465 kJ/kg for water at 15⁰C. In 1987 world energy consumption was estimated at 3.3 ´ 1017 kJ Incoming sunlight absorbed at 168 W/m2 at earth’s surface
Chemistry
10th Edition
ISBN:9781305957404
Author:Steven S. Zumdahl, Susan A. Zumdahl, Donald J. DeCoste
Publisher:Steven S. Zumdahl, Susan A. Zumdahl, Donald J. DeCoste
Chapter1: Chemical Foundations
Section: Chapter Questions
Problem 1RQ: Define and explain the differences between the following terms. a. law and theory b. theory and...
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- We have spent some time discussing reactions that occur in aqueous media and devoted some attention to the properties of water that make it unique. Now consider the power required to drive the hydrologic cycle, assuming that annual global rainfall averages 1 m across the approximately 5.1 ´ 1014 m2 of earth’s surface. What is the energy required to drive the hydrologic cycle? How does this compare with incoming solar radiation and world energy consumption? Consider the following data:
Latent heat of vaporization = 2465 kJ/kg for water at 15⁰C.
In 1987 world energy consumption was estimated at 3.3 ´ 1017 kJ
Incoming sunlight absorbed at 168 W/m2 at earth’s surface
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