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Explore how specific heat variances between land and water affect the radiative balance, heat equilibrium, and weather patterns in different locations. Understand the control needed to compare specific heat absorption rates in land versus water.
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AIM: How do differences in the specific heat of land and water control a locations weather and climate? Pre-Lab: Absorption & Radiation by Land & Water Radiative Balance: The ratio of absorption : radiation of insolation within the atmosphere Heat Equator: The locations with the warmest average surface temperatures on Earth at each longitude for a given day of the year http://www.geography.hunter.cuny.edu/~tbw/wc.notes/7.circ.atm/animations/WeatherPat.html
AIM: How do differences in the specific heat of land and water control a locations weather and climate? Concepts: A higher specific heat will cause a substance to warm (absorb) and cool (radiate) at a slower rate. (This means fast absorbers are also fast radiators) Q: What should be the “control” of the experiment if one is comparing the specific heat of land vs water? A: The energy each container receives