Environmental impacts: temperature, precipitation, sea level and circulation
Warming changes weather patterns, raises sea level (thermal expansion + meltwater) and alters ocean and wind circulation.
Global warming does far more than make the planet a little hotter — it changes the whole physical system. The syllabus expects you to state these environmental impacts and to be able to explain the most important ones.
| Environmental impact | What changes and why |
|---|---|
| Temperature | Average surface and ocean temperatures rise; heatwaves become more frequent and intense. |
| Precipitation | Rainfall patterns shift — some regions become wetter and others drier; rainfall can become more intense and less predictable. |
| Sea level | Sea level rises for two main reasons: (1) thermal expansion — water expands as it warms; and (2) meltwater added from melting land ice (glaciers and ice sheets). |
| Ocean circulation | Warming and added freshwater (meltwater) change water temperature, salinity and density, which can weaken or alter ocean currents that move heat around the planet. |
| Wind circulation | As temperature differences between regions change, large-scale wind patterns shift, changing where storms form and where rain falls. |
Why sea level rises (the exam favourite). Two processes work together. First, as the oceans absorb heat, the water expands — this is thermal expansion, and it raises sea level without any extra water being added. Second, ice stored on land (glaciers and the Greenland and Antarctic ice sheets) melts and runs into the sea, adding extra water. Crucially, melting sea ice (ice already floating on the ocean) does not raise sea level much, because floating ice already displaces its own weight of water — the big contributions are thermal expansion and land-ice meltwater.
Why circulation changes matter. Ocean and wind currents redistribute heat and moisture across the globe. When meltwater dilutes seawater or warming changes its density, currents can weaken or shift; shifting winds move the tracks of storms and rain belts. The result is that some regions get more extreme weather while others lose their reliable rainfall.
- Temperature rises; heatwaves become more frequent and intense.
- Precipitation patterns shift — some areas wetter, some drier, often more intense.
- Sea-level rise = thermal expansion of warming water + meltwater from land ice.
- Melting sea ice (floating) adds little to sea level; land ice is the key contributor.
- Changed temperature, salinity and density can weaken or shift ocean currents.
- Shifting wind patterns move where storms form and where rain falls.