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Harihar Rajaram

Researcher at Johns Hopkins University

Publications -  120
Citations -  4962

Harihar Rajaram is an academic researcher from Johns Hopkins University. The author has contributed to research in topics: Glacier & Ice sheet. The author has an hindex of 39, co-authored 114 publications receiving 3888 citations. Previous affiliations of Harihar Rajaram include University of Colorado Boulder.

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Importance and vulnerability of the world's water towers

TL;DR: The worldwide distribution and water supply of water towers (snowy or glacierized mountain ranges) is indexed, showing that the most important water towers are also the most vulnerable to socio-economic and climate-change stresses, with huge potential negative impacts on populations downstream.
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Solute transport in variable-aperture fractures: An investigation of the relative importance of Taylor dispersion and macrodispersion

TL;DR: In this article, a combination of physical experiments and computational simulations is used to test a theoretical model in which the effective longitudinal dispersion coefficient DL is expressed as a sum of the contributions of these three dispersive mechanisms.
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Saturated flow in a single fracture: evaluation of the Reynolds Equation in measured aperture fields

TL;DR: In this paper, the authors employed a light transmission technique with well-defined accuracy (approximately 1% error) to measure aperture fields at high spatial resolution (approximately 0.015 cm).
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Glacier crevasses: Observations, models, and mass balance implications

TL;DR: In this paper, the authors review the findings of approximately 60 years of in situ and remote sensing studies of glacier crevasses, as well as the three broad classes of numerical models now employed to simulate crevasse fracture.
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Influence of aperture variability on dissolutional growth of fissures in karst formations

TL;DR: The influence of aperture variability on dissolutional growth of fissures is investigated on the basis of two-dimensional numerical simulations in this paper, where the size of the fissure aperture before dissolution is modeled as a Gaussian stationary isotropic random field.