15 - Strålingspådriv

15 Kilde: IPCC SSP5 - 8.5 SSP3 - 7.0 SSP2 - 4.5 SSP1 - 2.6 SSP1 - 1.9 Total Total menneskeligskapt Volcanic Aerosols (direct effect ) Aerosols (indirect effects ) Land Use CO 2 CH 4 N 2 O Other WMGHG Tropospheric O 3 Stratospheric H 2 O Contrails Black carbon on snow Solar 2.8 W/m² Aerosoler Drivhuseffekt Strålingsbalanse
Set 3 www.climatefresk.org 15 Strålingsbalanse måler ubalansen mellom inngående og utgående energi fra jorda hvert sekund. I IPCCs femte hovedrapport vurderes strålingsbalansen til 2,8 W/m² (watt per kvadratmeter). 3,8 fra drivhuseffekten og - 1 fra aerosoler.

2
Causes

Aerosoler

Aerosoler

Aerosols cool down the climate.
Forsterket drivhuseffekt

Forsterket drivhuseffekt

The expression "Greenhouse Effect" is written on both sides (as of last version, October 2018).

1
Consequence

Strålingsbalanse

Strålingspådriv

The text behind card n14 allows no ambiguity. Therefore the 2 cards have to be skipped together or not at all.

2
Other possible causes

Avskoging

Avskoging

Smelting av sjøis

Smelting av sjøis

When the ice pack melts, a white surface is replaced by a dark blue surface, which has a lower albedo and therefore absorbs more energy. This relationship is not essential but it does allow another feedback loop of the game to be put forward.
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