| Popis: |
In this paper, a basic question is asked about a well-documented case study in Mexico: how well do we know Lake Patzcuaro? We address water balance as fundamental to the question. Past studies provide ambiguous explanations about the role of either underground infiltration and/or runoff, relative to the lake-level fluctuation. Thus, our suspicions over the database reliability led us to inspect historic records on water levels and climatic variables; check out the altitude of ground references, and analyze traces of runoff watercourses over the terrestrial basin by means of GIS. By making data re-arrangement and corrections, it became evident that the lake is subject to long-term cycles with ca. 40-year peaks, including short-term seasonal cycles within. Sensitivity to climatic conditions was determined, as well as the active influence of runoff as an important hydrologic component that contributes to cause serious damage to the land surface by erosion. Rearrangement of raw data highlights the occurrence of past misinterpretations founded on biased information. |
