Potential variation of Great Lakes water levels : a hydrologic response analysis

Hartmann, Holly C.

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The NOAA IR serves as an archival repository of NOAA-published products including scientific findings, journal articles, guidelines, recommendations, or other information authored or co-authored by NOAA or funded partners. As a repository, the NOAA IR retains documents in their original published format to ensure public access to scientific information.

i

Potential variation of Great Lakes water levels : a hydrologic response analysis

1988
By Hartmann, Holly C.
Series: NOAA technical memorandum ERL GLERL ; 68

[PDF-580.56 KB]

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Details:

Personal Author:

Hartmann, Holly C.
Corporate Authors:

Great Lakes Environmental Research Laboratory
NOAA Program & Office:

OAR (Oceanic and Atmospheric Research) ; GLERL (Great Lakes Environmental Research Laboratory)

OAR (Oceanic and Atmospheric Research) ; GLERL (Great Lakes Environmental Research Laboratory) Less -
Content Notes:

Holly C. Hartmann.

Distributed to depository libraries in microfiche.

"March 1988."

Also available online in PDF via the NOAA Central Library and the Great Lakes Environmental Research Laboratory website.

Includes bibliographical references (pages 28-30).
Keywords:

[+]

Climatic Factors Effect Of Human Beings On Hydrologic Models Hydrometeorology Monitoring Periodicity Water Levels
Series:

NOAA technical memorandum ERL GLERL ; 68 ; GLERL contribution ; no. 576

NOAA technical memorandum ERL GLERL ; 68 ; GLERL contribution ; no. 576 Less -
Document Type:

Technical Memorandum
Place as Subject:

Great Lakes (North America)
License:

https://creativecommons.org/publicdomain/zero/1.0/
Rights Information:

CC0 Public Domain
Compliance:

Library
Main Document Checksum:

[+]

urn:sha256:45603e4731b528ea452b438c57443222f41bfc1fde4d84a8506d4b793b2f15ae
Download URL:

https://repository.library.noaa.gov/view/noaa/11251/noaa_11251_DS1.pdf
File Type:

No Additional Files

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Potential variation of Great Lakes water levels : a hydrologic response analysis

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