Future Climate Change Flashcards

1
Q

Coupled Model Intercomparison Project 5 (CIMP5)

A
  • name of coordinated effort between global modeling centers to create a common set of climate change experiments
  • number 5 because the latest IPCC report is the 5th one to appear
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2
Q

RCP8.5

A
  • most aggressive scenario associated with radiative forcing
  • about 8.5 W/m2 in 2100
  • “business as usual scenario
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3
Q

RCP2.6

A
  • least aggressive scenario associated with radiative forcing
  • 2.6 W/m2 by 2100
  • mitigation forcing scenario
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4
Q

describe the warming commitment

A
  • we are already committed to significant warming because of the inertia of the climate system
  • the emissions we have already produced will stay in the atmosphere for hundreds of years even if we stop emitting today
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5
Q

describe the warming distribution under RCP8.5 & RCP2.6

A
  • more warming over continents than oceans
  • more warming over high latitudes than low latitudes
  • suppression of warming in the northern North Atlantic (thermohaline circulation)
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6
Q

why is there greater warming over continents than oceans

A
  • continents have a smaller effective heat capacity than the ocean –> warm more quickly than the ocean
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7
Q

describe the intensification of the hydrologic cycle

A

warming atmosphere –> increase in evaporation –> more water vapor to the atmosphere continuously –> atmosphere can hold a limited amount of vapor –> more rain

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8
Q

describe the net effect of the increase in precipitation

A
  • not a uniform increase
  • dry areas get drier
  • wet areas get wetter (Hadley Cell)
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9
Q

describe permafrost and where it is located

A
  • soil that remains below 32 degrees F for at least two years
  • mostly surrounding the Arctic ocean
  • characterized by an active surface layer, extending anywhere from a few centimeters to several meters deep, which thaws during the summer and refreezes during the winter
  • permafrost layer remains frozen
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10
Q

why is the loss of permafrost concerning

A
  • permafrost contains methane, which is released when the permafrost melts
  • has potential to enhance warming further since it’s a greenhouse gas
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