The key concept for Section 19.3. The thing that makes the current atmospheric warming problem urgent. Define climate change tipping points and give three examples. Briefly describe the possible effects of a warmer atmosphere on arctic sea ice and land-based ice, permafrost, and sea levels. Define ocean acidification and explain the way and the reason why it is occurring. Explain the way in which atmospheric warming, global drought, extreme weather, and an intensified water cycle are related. The possible effects of climate disruption on biodiversity, food production, and human health and economies. Pick three of these effects and describe the way in which each can become a part of positive feedback loop leading to increased climate disruption. Summarize the science community’s discussion of whether or not IPCC scientists were too conservative in their projections.

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Chapter 19, Problem 5CR

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The key concept for Section 19.3. The thing that makes the current atmospheric warming problem urgent. Define climate change tipping points and give three examples. Briefly describe the possible effects of a warmer atmosphere on arctic sea ice and land-based ice, permafrost, and sea levels. Define ocean acidification and explain the way and the reason why it is occurring. Explain the way in which atmospheric warming, global drought, extreme weather, and an intensified water cycle are related. The possible effects of climate disruption on biodiversity, food production, and human health and economies. Pick three of these effects and describe the way in which each can become a part of positive feedback loop leading to increased climate disruption. Summarize the science community’s discussion of whether or not IPCC scientists were too conservative in their projections.

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Discussion Question: Atmospheric Water & Weather A+ This chapter beautifully focuses on water from the small molecular scale to large-scale weather patterns. The surplus of heat at the equator and the deficit at the Poles drives our atmospheric instability. Instability is a good thing! Without the unstable conditions, there would not be any atmospheric motion. The overheating of the equator pumps atmospheric uplift. As the air rises into lower pressures, it expands and cools... adiabatic cooling! The air migrates north and south and becomes denser than the surrounding air and sinks. The sinking air enters higher pressures and creates the subtropical high pressures and adiabatic heating...whaaaa-la! We have Hadley Cells! Not to mention, the Rainforests and World's largest deserts too! We now can imagine the Hadley cells in three-dimensions. They more or less "sandwich" the equator during the spring and fall equinoxes. However, what happens in the summer and winter? mP Maritime polar…