Reanalysis is a scientific method used in climatology and meteorology to produce comprehensive and consistent datasets of past weather and climate conditions. It involves the assimilation of various observational data sources, such as weather station records, satellite measurements, and ocean buoys, into numerical weather prediction models. The goal of reanalysis is to create a long-term, coherent dataset that enables researchers to study climate patterns, trends, and variability over time.
Articles by others on the same topic
There are currently no matching articles.