14 - Rozpočítanie energie

Rozpočítanie energie Topiaci sa ľad Pôda 3 % 3 % Oceán Atmosféra 1 % 93 % Source: IPCC 14
Set 3 www.climatefresk.org 14 Tento graf znázorňuje kam sa podeje energia nazbieraná na zemi kvôli radiačnému pôsobeniu: otepľuje oceán, roztápa ľad, rozptyľuje sa do pôdy a otepľuje atmosféru.

2
Causes

Radiačné pôsobenie

Radiačné pôsobenie

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

Hydráty metánu

Heat is absorbed at the surface of the ocean. Thermohaline circulation helps mix watersurface and deep ocean which is essential to the absoption of energy by the ocean.

5
Consequences

Topenie ľadovcov

Rozpočítanie energie


Nárast teploty vody

Rozpočítanie energie


Topenie morského ľadu

Rozpočítanie energie


Topenie pevninských ľadovcov

Rozpočítanie energie


Nárast teplôt

Rozpočítanie energie

As mentionned on card 21, this is the temperature of the air, above ground, in average on the Earth.

1
Other possible consequence

Permafrost

Rozpočítanie energie

If we take the idea of energy conservation all the way, we can link the energy budget to the thawing of permafrost.

1
Wrong cause

Absorbéry uhlíka

Absorbéry uhlíka

The idea here is not to say there is no link between these two cards, but to make sure they are not mixed up. The carbon sinks card tells us where the carbon goes. The energy budget card tells us where the excess energy goes. Both distribute something, but not the same thing. To make it even more confusing, the atmosphere and the ocean are present in both.
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