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Daniel E. Ibarra

Researcher at University of California, Berkeley

Publications -  85
Citations -  1455

Daniel E. Ibarra is an academic researcher from University of California, Berkeley. The author has contributed to research in topics: Geology & Weathering. The author has an hindex of 18, co-authored 52 publications receiving 904 citations. Previous affiliations of Daniel E. Ibarra include Brown University & Planetary Science Institute.

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Steering of westerly storms over western North America at the Last Glacial Maximum

TL;DR: The Last Glacial Maximum hydroclimate over western North America differed from the modern climate, and a proxy-model comparison suggests that the glacial storm track was squeezed and steered by atmospheric high-pressure systems as mentioned in this paper.
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Differential weathering of basaltic and granitic catchments from concentration–discharge relationships

TL;DR: In this paper, the authors quantify the processes that determine catchment-scale solute fluxes for two lithologic end-members (basalt and granite) by applying a recently developed solute production model that links weathering fluxes to both discharge and the reactivity of the weathering material.
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Neogene cooling driven by land surface reactivity rather than increased weathering fluxes

TL;DR: A parsimonious carbon cycle model constrained by weathering-sensitive isotopic tracers reveals that long-term cooling in the Neogene period reflects a change in how surface denudation is partitioned into weathering and erosion.
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Stable runoff and weathering fluxes into the oceans over Quaternary climate cycles

TL;DR: In this article, a beryllium-based proxy for weathering shows minimal variations in the input of silicate weathering products to the oceans for the past two million years.
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Rise and fall of late Pleistocene pluvial lakes in response to reduced evaporation and precipitation: Evidence from Lake Surprise, California

TL;DR: A detailed analysis of lake hydrography and constitutive relationships describing the water balance to determine the influence of precipitation, evaporation, temperature, and seasonal insolation on past lake levels is presented in this article.