Ecological Dynamics of Watersheds

Olsen, Sigurd; Chapman, Douglas G.

doi:10.2307/1296078

Cited by 3 publications

(2 citation statements)

References 11 publications

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“…Mid-latitude estuaries undergo wide swings in productivity because of seasonal temperature fluctuations and variations of the amount of runoff (Fisher & Likens 1972, Olsen & Chapman 1972. Meteorological conditions, the dynamics of the atmosphere-ocean system, and the geographic arrangement of mountain ranges and coasts as described in Chapter 6 dictate most of those regions.…”

Section: Physical Properties Of the Marine Environmentmentioning

confidence: 99%

Patterns of Life

Mielke¹

1989

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and the skilled people at Unwin Hyman were steadfast and helpful at every point in the writing and publishing craft. To all the above people my sincerest thanks. I profited from their interest and assistance and the book has been greatly improved and enriched as a result of their efforts and helpful advice. Whatever errors and deficiencies that remain are not theirs, but mine.I wish to dedicate this book to my students who nurtured thinking about patterns of life and to my daughter Beverly Ann who is a constant inspiration and motivates thoughts about now and the future.

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Section: Physical Properties Of the Marine Environmentmentioning

confidence: 99%

Patterns of Life

Mielke¹

1989

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“…Stream chemistry measurements at catchment outlets have been used to understand linkages between terrestrial and aquatic processes since the 1960's (Bormann & Likens, 1967; Dale, 1970; Mann, 1969; Odum, 1969; Olsen & Chapman, 1972). Early biogeochemistry research quantified catchment nutrient retention and loss dynamics by comparing nutrient inputs versus outputs (Fisher & Likens, 1973; McDowell & Likens, 1988), focusing on a whole‐ecosystem approach.…”

Section: Introductionmentioning

confidence: 99%

Catchment concentration–discharge relationships across temporal scales: A review

Speir,

Rose,

Blaszczak

et al. 2023

WIREs Water

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Processes that drive variability in catchment solute sourcing, transformation, and transport can be investigated using concentration–discharge (C–Q) relationships. These relationships reflect catchment and in‐stream processes operating across nested temporal scales, incorporating both short and long‐term patterns. Scientists can therefore leverage catchment‐scale C–Q datasets to identify and distinguish among the underlying meteorological, biological, and geological processes that drive solute export patterns from catchments and influence the shape of their respective C–Q relationships. We have synthesized current knowledge regarding the influence of biological, geological, and meteorological processes on C–Q patterns for various solute types across diel to decadal time scales. We identify cross‐scale linkages and tools researchers can use to explore these interactions across time scales. Finally, we identify knowledge gaps in our understanding of C–Q temporal dynamics as reflections of catchment and in‐stream processes. We also lay the foundation for developing an integrated approach to investigate cross‐scale linkages in the temporal dynamics of C–Q relationships, reflecting catchment biogeochemical processes and the effects of environmental change on water quality.This article is categorized under: Science of Water > Hydrological Processes Science of Water > Water Quality Science of Water > Water and Environmental Change

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Forests, man and water

Moore

1985

International Journal of Environmental Studies

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Ecological Dynamics of Watersheds

Cited by 3 publications

References 11 publications

Patterns of Life

Patterns of Life

Catchment concentration–discharge relationships across temporal scales: A review

Forests, man and water

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