A study of long-term environmental fluctuations in the Chesapeake Bay region

A time series of monthly mean values of temperature measurements (1952-1981) for Gloucester Point, Virginia, U.S.A. and Vardo In Northern Norway are described and the results of an eigenfunction analysis are presented. Seasonal, year-to-year and long term changes of salinlty measurements (1960-1977)...

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Main Authors: Leinebo, Reidar S., Evans, David A.
Format: Text
Language:unknown
Published: W&M ScholarWorks 1984
Subjects:
Online Access:https://scholarworks.wm.edu/reports/2772
https://scholarworks.wm.edu/context/reports/article/3760/viewcontent/Longterm_Environmental_Flucations_Chesapeake.pdf
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spelling ftwilliammarycol:oai:scholarworks.wm.edu:reports-3760 2023-06-11T04:10:33+02:00 A study of long-term environmental fluctuations in the Chesapeake Bay region Leinebo, Reidar S. Evans, David A. 1984-01-01T08:00:00Z application/pdf https://scholarworks.wm.edu/reports/2772 https://scholarworks.wm.edu/context/reports/article/3760/viewcontent/Longterm_Environmental_Flucations_Chesapeake.pdf unknown W&M ScholarWorks https://scholarworks.wm.edu/reports/2772 https://scholarworks.wm.edu/context/reports/article/3760/viewcontent/Longterm_Environmental_Flucations_Chesapeake.pdf Reports Water temperature -- Chesapeake Bay (Md. and Va.) Salinity -- Chesapeake Bay (Md. and Va.) Water temperature -- Barents Sea Salinity -- Barents Sea Research and Technical Reports Environmental Monitoring text 1984 ftwilliammarycol 2023-05-04T17:50:52Z A time series of monthly mean values of temperature measurements (1952-1981) for Gloucester Point, Virginia, U.S.A. and Vardo In Northern Norway are described and the results of an eigenfunction analysis are presented. Seasonal, year-to-year and long term changes of salinlty measurements (1960-1977) for Gloucester Point and monthly mean stream-flow values (1951-1982) are also described. Commerclal Catch data from Virginia for menhaden, bluefish and Atlantic croaker shows reasonable correlation with cllmatlc changes. The time around 1965 was a cold period with high sallnlty and low streamflow. The same period was also cold In Northern Norway (Europe). Around 1974 was a period of high temperature with low salinlty and high stream-flow caused mainly by ml Id winters. This period coincided with a warm period In Northern Norway. The long-term periodic temperature variation at Gloucester Point Is related to general climatlc variations In the Northern Hemisphere. VIMS Pier temperatures, salinity readings. Text Barents Sea Northern Norway W&M ScholarWorks Barents Sea Norway Vardo ENVELOPE(17.670,17.670,68.533,68.533)
institution Open Polar
collection W&M ScholarWorks
op_collection_id ftwilliammarycol
language unknown
topic Water temperature -- Chesapeake Bay (Md. and Va.)
Salinity -- Chesapeake Bay (Md. and Va.)
Water temperature -- Barents Sea
Salinity -- Barents Sea
Research and Technical Reports
Environmental Monitoring
spellingShingle Water temperature -- Chesapeake Bay (Md. and Va.)
Salinity -- Chesapeake Bay (Md. and Va.)
Water temperature -- Barents Sea
Salinity -- Barents Sea
Research and Technical Reports
Environmental Monitoring
Leinebo, Reidar S.
Evans, David A.
A study of long-term environmental fluctuations in the Chesapeake Bay region
topic_facet Water temperature -- Chesapeake Bay (Md. and Va.)
Salinity -- Chesapeake Bay (Md. and Va.)
Water temperature -- Barents Sea
Salinity -- Barents Sea
Research and Technical Reports
Environmental Monitoring
description A time series of monthly mean values of temperature measurements (1952-1981) for Gloucester Point, Virginia, U.S.A. and Vardo In Northern Norway are described and the results of an eigenfunction analysis are presented. Seasonal, year-to-year and long term changes of salinlty measurements (1960-1977) for Gloucester Point and monthly mean stream-flow values (1951-1982) are also described. Commerclal Catch data from Virginia for menhaden, bluefish and Atlantic croaker shows reasonable correlation with cllmatlc changes. The time around 1965 was a cold period with high sallnlty and low streamflow. The same period was also cold In Northern Norway (Europe). Around 1974 was a period of high temperature with low salinlty and high stream-flow caused mainly by ml Id winters. This period coincided with a warm period In Northern Norway. The long-term periodic temperature variation at Gloucester Point Is related to general climatlc variations In the Northern Hemisphere. VIMS Pier temperatures, salinity readings.
format Text
author Leinebo, Reidar S.
Evans, David A.
author_facet Leinebo, Reidar S.
Evans, David A.
author_sort Leinebo, Reidar S.
title A study of long-term environmental fluctuations in the Chesapeake Bay region
title_short A study of long-term environmental fluctuations in the Chesapeake Bay region
title_full A study of long-term environmental fluctuations in the Chesapeake Bay region
title_fullStr A study of long-term environmental fluctuations in the Chesapeake Bay region
title_full_unstemmed A study of long-term environmental fluctuations in the Chesapeake Bay region
title_sort study of long-term environmental fluctuations in the chesapeake bay region
publisher W&M ScholarWorks
publishDate 1984
url https://scholarworks.wm.edu/reports/2772
https://scholarworks.wm.edu/context/reports/article/3760/viewcontent/Longterm_Environmental_Flucations_Chesapeake.pdf
long_lat ENVELOPE(17.670,17.670,68.533,68.533)
geographic Barents Sea
Norway
Vardo
geographic_facet Barents Sea
Norway
Vardo
genre Barents Sea
Northern Norway
genre_facet Barents Sea
Northern Norway
op_source Reports
op_relation https://scholarworks.wm.edu/reports/2772
https://scholarworks.wm.edu/context/reports/article/3760/viewcontent/Longterm_Environmental_Flucations_Chesapeake.pdf
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