Ice cores contain tiny bubbles that contain a sample of the atmosphere from that time period. By studying the ice bubbles, it is possible to reconstruct the composition of the atmosphere at that time and thus the climate.
Tree cores are small and skinny if it was cold that year.
pudding
Warm and cool ocean currents influence the climate. The UK is a good example, being affected by the warm Gulf Stream.
Paleoclimate.
i dont know what is it
sea level is rising
occur today only in a specific environment
to determent past climates
Tree cores are small and skinny if it was cold that year.
pudding
General circulation models are not typically used as direct evidence of past climates due to their forward-looking nature in simulating future climate scenarios. Instead, proxies like ice cores, tree rings, and sediment layers are used to reconstruct past climates. General circulation models are more commonly used to study and project future climate changes based on various input parameters and scenarios.
The best evidence you have of past climate is written almanacs and weather reports. Almanacs have been kept for centuries and well document the climate.
Evidence for past glaciations includes glacial landforms like moraines and drumlins, glacial striations on bedrock caused by the movement of glaciers, and the presence of glacial erratics, which are large rocks transported by glaciers and deposited in areas where they are not native. Additionally, the study of ice cores from polar ice sheets provides a record of past climate conditions and the extent of glaciations.
Warm and cool ocean currents influence the climate. The UK is a good example, being affected by the warm Gulf Stream.
Paleoclimate.
i dont know what is it
Studying tree rings, Dendrochronology is one way.Studying ice cores is another, in particular looking at the ratio of 16O to 18O. This ratio (in precipitated water) is sensitive to the ambient temperature.