Weather and climate
Cloud shapes, daylight and climate zones become easier to distinguish when you can change the date, latitude and temperature in a model.
- 1CloudsA small cumulus cloud 1 km across holds about 500 tonnes of water and still floats. Learn how clouds form, the ten cloud types in the WMO International Cloud Atlas and the heights they live at, and what each one tells you about the weather. The 3D block puts cirrus, cumulus, stratus and cumulonimbus at their real heights.6 Units
- 2Seasons and climate zonesEarth is closest to the Sun in early January, in the middle of the northern winter. Seasons come from the 23.44° tilt of Earth's axis. Move the Earth around its orbit, pick a latitude and read off day length and the height of the noon Sun, then see how those numbers sort the world into climate zones.6 Units
The sky above a particular place
Looking up at a cloud and comparing summer with winter involve different scales of explanation. The cloud course follows water in the air and the forms clouds take. The seasons course asks how date and latitude affect daylight, then considers climate zones. Read them together to connect a familiar view of the sky with the geometry behind seasonal changes. Keep a description of the cloud you see separate from a claim about the climate of the place where you are standing.
Cloud forms before climate groups
Start with Clouds. The opening units explain cloud formation and naming. Low clouds include cumulus, stratus and stratocumulus; another unit distinguishes middle and high clouds. Cumulonimbus receives its own treatment as the thunderstorm cloud, followed by a unit on reading the sky. Learn the differences in shape and height together, so a name points to features you can actually describe rather than just a word on a flashcard.
Then read Seasons and climate zones. It begins with why seasons happen and how day length varies with latitude. Polar day and polar night, the tropics and the subsolar point make the geometry more specific. The course introduces the Köppen climate groups and ends with seasons in the southern hemisphere. That last comparison is a useful check on explanations built only around the seasons at home.
Compare two settings and hold one fixed
The cloud menu lets you switch between forms in the water-cycle model. Compare the low stratus layer with high cirrus and the vertical extent of cumulonimbus. In the final cloud unit, start at 25 °C and change to 5 °C, watching the model rather than assuming the picture will stay the same. Record which setting you changed and what the scene shows.
In the seasons model, move the date slider at a fixed latitude, then keep the date fixed while changing latitude. The close view makes differences in daylight easier to inspect. Compare a northern setting with the southern setting used in the final unit. Changing one input at a time helps you explain which result belongs to the date and which belongs to the observer’s position.
Explanations to check against the model
Do not use one season’s weather as the definition of a climate zone. The course separates climate groups from the mechanism producing seasons. Likewise, learning a cloud name should not replace describing its height and form. Return to the formation unit when a label has become detached from the process. Use the unit questions to test your explanation without the diagram in front of you, then reopen the model to check the part you could not explain. The aim is an account that still makes sense when the location or date changes.
Questions about this subject
Are clouds made of water vapour?
Water vapour is invisible, whereas clouds are visible because tiny liquid droplets or ice crystals scatter sunlight. Vapour condenses onto small particles such as dust, salt or smoke to form droplets. Calling a cloud a patch of visible gas misses the change of state that makes it possible to see the cloud at all. Clouds
Why does rising air form clouds?
As air rises, the surrounding pressure falls and the air expands, which cools it. Cooling to the dew point brings it to saturation and allows water vapour to condense. Unsaturated rising air cools at about 9.8 degrees Celsius per kilometre, so lifting air over mountains or along a front can produce cloud without adding more water to it. Clouds
How can a cloud containing tonnes of water stay in the sky?
Its water is spread as very small droplets through a huge volume of air rather than gathered into one heavy object. Those droplets fall slowly enough for gentle updrafts to keep them aloft. A one-kilometre cube of typical cumulus contains about five hundred tonnes of water, but rain falls only after droplets grow large enough to fall out. Clouds
Why can a cloud disappear without producing rain?
Droplets can evaporate where a cloud mixes with drier surrounding air. New droplets may still be forming inside rising air, so the visible cloud reflects a changing balance between condensation and evaporation. A cumulus can grow and disappear within twenty minutes without all its water needing to reach the ground as rain first. Clouds
What do cirrus, cumulus and stratus mean?
The names describe form: cirrus suggests a curl or wisp of hair, cumulus a heap, and stratus a layer or sheet. They distinguish thin high streaks, puffy heaps and flatter cloud layers rather than simply listing colours. In combined names, nimbo or nimbus indicates a rain cloud, while alto identifies middle-level relatives of lower cloud forms. Clouds