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Ishi Buffam

Researcher at University of Cincinnati

Publications -  74
Citations -  6990

Ishi Buffam is an academic researcher from University of Cincinnati. The author has contributed to research in topics: Dissolved organic carbon & Green roof. The author has an hindex of 37, co-authored 70 publications receiving 6271 citations. Previous affiliations of Ishi Buffam include University of Wisconsin-Madison & Marine Biological Laboratory.

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Energy exchange and water budget partitioning in a boreal minerogenic mire

TL;DR: Peichl et al. as mentioned in this paper investigated patterns and controls of the seasonal and inter-annual variations in energy fluxes and partitioning of the water budget (i.e., precipitation, P; evapotranspiration, ET; discharge, Q; and soil water storage, Delta S) over five years (2001-2005).
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Patterns and dynamics of dissolved organic carbon (DOC) in boreal streams: The role of processes, connectivity, and scaling

TL;DR: In this article, the Krycklan Catchment Study was used to study the role of hydrological mechanisms, connectivity and scaling for understanding the pattern and dynamics of surface water DOC across complex landscapes.
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Ecosystem Consequences of Changing Inputs of Terrestrial Dissolved Organic Matter to Lakes: Current Knowledge and Future Challenges

TL;DR: In this paper, the authors review the substantial literature describing tDOM effects on lakes and ongoing changes in tDOM inputs, and identify and provide examples of four major challenges that limit predictions about the implications of tDOM change for lakes, as follows: First, it is currently difficult to forecast future t DOM inputs for particular lakes or lake regions, and our holistic understanding of those effects is still rudimentary.
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Seasonal TOC export from seven boreal catchments in northern Sweden

TL;DR: In this article, the authors examine spatial and temporal variations in streamwater TOC export and its relationship with catchment characteristics, and suggest that the smaller relative importance of the spring runoff period for the annual TOC output from wetland dominated catchments is a result of the hydrological flow paths associated with the snow melt period.