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climate change
Climate change is a change in the statistical distribution of meteorological patterns when this change lasts for an extended period of time. Climate change can refer to a change in average weather conditions or to changes in weather in the context of long-term average conditions. Climate change is caused by factors such as biotic processes, variations in solar radiation received by the Earth, plate tectonics and volcanic eruptions. Certain human activities have been identified as the main causes of ongoing climate change, often referred to as global warming.
Scientists are actively working to understand past and future climate, using theoretical observations and models. A climate record - which extends far into the Earth's past - was initiated and continued on the basis of geological evidence from drill temperature profiles, cores from deep ice accumulations, flora and fauna records, glacial and periglacial processes, - stable isotopes and other analyzes of sediment layers and records of past sea levels. The latest data is provided by the instrumental record. General circulation models, based on the physical sciences, are often used in theoretical approaches to match past climate data, make future projections, and link the causes and effects of climate change.