Synoptic Climatology for the Susquehanna River Basin

Objectives

SRBEX research in synoptic climatology has three current foci:

  1. Determining representative circulation patterns and their hydrologic response;

  2. Establishing empirical relationships between the response of watersheds with differing scales and synoptic forcing;

  3. Developing techniques to monitor large-scale climatic variation.

Current Activities

The first focus arises from the assumption by the SRBEX linked-modeling efforts that there is a strong causal relationship between the atmospheric circulation and the hydrologic response of the basin. Many of the simulations linking the atmosphere and basin hydrology rely on observed events believed to be typical. Yet no methodology has been developed to determine either the representativeness of the circulation patterns producing a significant hydrologic response, or the representativeness of the hydrologic response to a given storm system. In preliminary research, Yarnal and Draves (1993) used composite pressure patterns and storm tracks to show that the largest runoff events in the Susquehanna River Basin (SRB) may result from characteristic sequences of synoptic patterns. Consequently, Frakes and Yarnal (1994) have developed a technique for determining unique circulation events and those storm patterns that typically produce a strong hydrologic response in the basin. These data can also be used to understand which hydrologic responses to a given circulation event are representative or not. The results suggest that synoptic climatology is a useful tool for defining model scenarios and model verification in global-change experiments.

SRBEX also seeks to identify how watersheds of differing scales respond to forcing by weather systems. The second focus of SRBEX synoptic climatology addresses the observational component of this objective. Frakes and Yarnal (1995) are creating a catalog of daily eigenvector-based synoptic map patterns, plus indices based on these patterns (Yarnal, 1993) for the period 1946-1994. Quarterly updates of the catalog will be available in hard copy and over the Internet starting in the last quarter of 1995. These data will be integral to developing long-range forecasts of basin climate and hydrology.

Results


Last change: 3 May 1995, R. A. White / raw@essc.psu.edu