Search results for "surface hydrology"

showing 2 items of 2 documents

Standard Asymptotic Response and Expected Runoff from Curve Number Theory

2015

The Standard Asymptotic response is a common finding with rainfall-runoff analysis with the Curve Number method. Widely-observed in data analyses, it is the secondary relationship between the data-defined CN and the causative rainfall P, for which the empirical fitting equation CN(P) = CN∞+ (100-CN∞)exp(-kP) has been found to fit well. This is an unexpected variation in the handbook methodology. It is investigated here on a “theoretical” basis by using the handbook tabled values of CN for the three AMC classes, I, II, and III; the storm-to-storm S (=1000/CN-10); and the observed 12-50-88 percent conditional probabilities for the ARC classes. With this, and treating S as a variable across th…

curve numberStatisticssurface hydrologyrunoffRunoff curve numberSurface runoffMathematics
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WATER MASSES EXCHANGE THROUGH THE STRAIT OF SICILY DURING THE LAST DEGLACIAL PERIOD AND THE HOLOCENE

2022

The main goal of this thesis is to explore the inter-basin connection between the eastern and the western Mediterranean (E- and W-Med, respectively) during the last deglacial and Holocene periods (last 15 kyr). The thesis is based on the study of a sediment core recovered at the west flank of Sicily channel (W-Sicily), strategically located under the current path of the surface Atlantic waters and directly below the present-day hydrographic boundary layer between the Eastern Mediterranean Sourced Water (EMSW) and the Western Mediterranean Deep Water (WMDW). This key location allow to explore past changes in both surface and deep water exchange between the E and the W-Med. In this thesis, a …

deep hydrologyNeodymiumAfrican Humid Period.HoloceneEastern Mediterranean basinMediterranean Thermohaline circulationlast Sapropel (S1)Western Mediterranean Deep WaterYounger DryaSettore GEO/01 - Paleontologia E Paleoecologialate deglacialsurface hydrologyEastern Mediterranean Sourced WaterMediterranean SeaWestern Mediterranean basin
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