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Sunday, July 26, 2020 | History

2 edition of Simulation of ice-cover growth and decay in one dimension on the upper St. Lawrence River found in the catalog.

Simulation of ice-cover growth and decay in one dimension on the upper St. Lawrence River

Gordon M. Greene

Simulation of ice-cover growth and decay in one dimension on the upper St. Lawrence River

by Gordon M. Greene

  • 187 Want to read
  • 17 Currently reading

Published by U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories in Ann Arbor, Mich .
Written in English

    Subjects:
  • Ice on rivers, lakes, etc. -- Saint Lawrence River -- Simulation methods.

  • Edition Notes

    StatementGordon M. Greene.
    SeriesNOAA technical memorandum ERL GLERL -- 36
    ContributionsGreat Lakes Environmental Research Laboratory.
    The Physical Object
    Paginationv, 82 p. :
    Number of Pages82
    ID Numbers
    Open LibraryOL17072921M

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Simulation of ice-cover growth and decay in one dimension on the upper St. Lawrence River by Gordon M. Greene Download PDF EPUB FB2

Dec 03,  · Simulation of ice-cover growth and decay in one dimension on the upper St. Lawrence RiverU.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories. Get this from a library. Simulation of ice-cover growth and decay in one dimension on the upper St.

Lawrence River. [Gordon M Greene; Great Lakes Environmental Research Laboratory,]. A unified degree-day method for river ice cover thickness simulation. Simulation of ice-cover growth and decay in one-dimension on the Upper St.

Lawrence River. NOAA ' TM ERL GLERL, Great. Simulation of ice-cover growth and decay in one dimension on the upper. Use of a Water Temperature-Ecological Model to Simulate Global Warming Effects on a Lake Ecosystem. Simulation of ice-cover growth and decay in one dimension on the upper St.

Lawrence River. NOAA Technical Memoranduni ERL CLERL, Cited by: 1. Greene GM () Simulation of ice-cover growth and decay in one dimension on the upper St. Lawrence River. NoAA Technical Memorandum Erl GLERL Google Scholar. Carlson RE () A trophic state index for lakes. Search book. Search within book.

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Recent video and acoustic surveys of the upper St. Clair River, as part of the International Upper Great Lakes Study, have revealed new information about the geology, morphology and substrate of this unusual, non-alluvial, river. The upper km of the river is underlain by a considerable thickness of fluvio-glacial gravel, which thins.

An approximation on which we will rely in this report is “pattern scaling”, in which a robust pattern of climate change is assumed to exist that describes the geographical and seasonal structure of the temperature response that does not depend on climate sensitivity or on.

At present such models require inputs such as ice cover and other parameters. The model used in the present work uses only irradiance and volcanic aerosol estimates, modeling the ice cover by first modeling the glacial volume and area.

The net annual continental ice accumulation rate must be integrated to obtain the global glacial volume. Research on changes in the climate system on decade-to-century timescales has achieved notable successes in the past decade. The effective use of the paleoclimate record has revealed attributes of natural climate variability and has provided a context for the study of present and future global change.

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Phytoplankton dynamics in a chain of subtropical blackwater lakes: the Upper St. Johns River, Florida, USA. Lake Reserv. Manage. Spatial and seasonal patterns in phytoplankton biovolume and community composition were examined for a chain of lakes in the Upper St.

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