Temporal climate variations result from a wide range of physical, chemical, and biological processes, including chaotic or near-chaotic fluid dynamics, complex radiative and moist-thermodynamic processes, tropical-extratropical interactions, ocean-air interactions, and the responses of terrestrial ecosystems to atmospheric forcings. Understanding the Nation's hydroclimate, water resources, and water-related hazards requires improved understanding and integration of these processes and interactions into interpretations and procedures. Despite the almost overwhelming complexity of these processes, the fields of statistical and dynamic climatology currently are providing many examples of how climate processes can be interpreted, modeled, and predicted by using physically and statistically based models. The climate system offers numerous possibilities for improving the understanding of hydrologic and water-resources systems, and opportunities for converting improvements in climatological understanding into improvements in hydrologic prediction.
An integral part of the U.S. Geological Survey's mission to appraise the Nation's water resources and provide hydrologic information for managing them must be the extraction of as much order and predictability from the Nation's hydroclimate as possible. The primary objectives of this project are to identify (1) climatologically induced relations within the Nation's hydrologic and water resource system, (2) recurring hydroclimatological patterns and climatologically imposed limits on hydrologic and water resource systems, (3) conditions leading to climatological extremes and resultant hydrologic hazards, and (4) regional and global climatic precursors of hydrologic events and hazards. Products of this project contribute directly to more accurate appraisals and management of the Nation's water resources and water-related hazards.