EdGCM Teaching Tips

2.Comparing different elements within a specific scenario

Global warming experiment as an example

2.1. Surface temperature and sea surface temperature

Surface air temperatureSea surface temperature
You will see the delay of warming of sea surface. Also, the temperature rise in surface air is larger than sea surface. You may ask the reason why to students.

2.2 Planetary albedo and total cloud cover

Planetary albedoTotal cloud cover
You can confirm that albedo decrease was not caused by the decrease of the total cloud cover. You can see that the decrease of total cloud cover starts far later than planetary albedo starting.

2.3 Planetary albedo and ground albedo

Planetary albedoGround albedo
You can confirm that planetary albedo decrease delayed to the ground albedo decrease.

2.4 Snow cover and ocean ice cover

Snow coverOcean ice cover
These two are very similar decrease. They decrease from very early time of the simulation. Also, you can confirm that decrease of snow cover and ocean ice cover speed up at the middle of the simulation. Also, the curves of snow cover and ocean ice cover are very similar to those of planetary and ground albedos.

2.5 Precipitation and water content

PrecipitationWater content
These two elements start to increase after 2000. However, the increase rate of water content is larger than water content. The curve of water content is similar to surface air temperature. Additional information may be required to discuss further such as saturation vapor pressure table and graph.

2.6 Precipitation and evaporation

PrecipitationEvaporation
They show very similar change and amount. That means evaporation is basically balanced with precipitation. Therefore, the increase of water content means that increase in evaporation is larger than precipitation.
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