Faculty Advisor

Dr. Thomas Brubaker

Department

Geosciences

Presentation Date

4-13-2017

Document Type

Poster

Abstract

Precipitation is the ultimate source of all surface and groundwater recharge. Stable oxygen and hydrogen isotope investigation of precipitation has a long history. The factors controlling these stable isotopes are well known and include mean annual temperature, amount of precipitation, altitude and air mass trajectory (Dansgaard, 1964; Yurtsever and Gat, 1981).

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