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Katerina Michaelides
Researcher at University of Bristol
Publications - 57
Citations - 1025
Katerina Michaelides is an academic researcher from University of Bristol. The author has contributed to research in topics: Surface runoff & Erosion. The author has an hindex of 18, co-authored 45 publications receiving 781 citations. Previous affiliations of Katerina Michaelides include University of California, Santa Barbara.
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Modelling the effects of hillslope–channel coupling on catchment hydrological response
TL;DR: In this paper, a two-dimensional hydrological model has been developed that accounts for dynamic interactions between hillslope and channel flows, specifically designed for semi-arid areas dominated by Hortonian overland flow, and has a dynamically active channel belt.
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Connectivity as a concept for characterising hydrological behaviour
TL;DR: This commentary discusses the importance and meaning of connectivity and advocates the use of geostatistical connectivity to provide a methodological framework within a hydrological context that transcends individual complexities inHydrological response.
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Vegetation controls on small-scale runoff and erosion dynamics in a degrading dryland environment
TL;DR: In this paper, the authors investigated the control of vegetation on runoff and erosion dynamics in the dryland environment of Jornada, New Mexico, USA, and found that the primary vegetation control is the shrub type and canopy density, which directly affects the local microtopographic gradient of mounds beneath the shrubs.
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Aridity is expressed in river topography globally.
Shiuan-An Chen,Katerina Michaelides,Stuart W. D. Grieve,Michael Bliss Singer,Michael Bliss Singer +4 more
TL;DR: A global dataset of river longitudinal profiles is presented and it is shown that river profiles become straighter with increasing aridity and numerical modelling suggests that this can be explained by rainfall–runoff regimes in different climate zones.
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Surface water connectivity dynamics of a large scale extreme flood
TL;DR: In this paper, the authors quantify surface water connectivity geostatistically as an objectively measurable characteristic of an observed flood event using a time series of MODIS (Moderate Resolution Imaging Spectroradiometer) surface water product for an extreme large scale flood event (11,000 km 2 flooded area and 6 months duration) during 2011 in Bangkok, Thailand.