Author: George P. Knapp
Publisher:
ISBN:
Category : Hydrography
Languages : en
Pages : 107
Book Description
Hydrographic Data from R.V. Oceanus Cruise 133, Leg VII
Author: George P. Knapp
Publisher:
ISBN:
Category : Hydrography
Languages : en
Pages : 107
Book Description
Publisher:
ISBN:
Category : Hydrography
Languages : en
Pages : 107
Book Description
Efficient Representation of the Hydrographic Structure of the North Atlantic Ocean and Aspects of the Circulation from Objective Methods
Author: Ichiro Fukumori
Publisher:
ISBN:
Category : North Atlantic Ocean
Languages : en
Pages : 674
Book Description
Publisher:
ISBN:
Category : North Atlantic Ocean
Languages : en
Pages : 674
Book Description
Journal of Physical Oceanography
Bulletin of Marine Science of the Gulf and Caribbean
Hydrographic Data from R/V Endeavor Cruise #143
Author:
Publisher:
ISBN:
Category : Chemical oceanography
Languages : en
Pages : 578
Book Description
Hydrographic data collected during R/V Endeavor cruise 143 is presented as a preliminary study of subduction in the northeast Atlantic south of the Azores Front. The front is clearly defined at the northern end of CTD section #1 which also shows a layer of 16-18°C water subducted to the south. Section #2, 280 km to the east, is dominated by a large cyclonic ring with characteristics similar to 'eastern' rings reported earlier . An anomalously salty parcel of Mediterranean water in this section is typical of highly saline lenses seen in the Canary Basin.
Publisher:
ISBN:
Category : Chemical oceanography
Languages : en
Pages : 578
Book Description
Hydrographic data collected during R/V Endeavor cruise 143 is presented as a preliminary study of subduction in the northeast Atlantic south of the Azores Front. The front is clearly defined at the northern end of CTD section #1 which also shows a layer of 16-18°C water subducted to the south. Section #2, 280 km to the east, is dominated by a large cyclonic ring with characteristics similar to 'eastern' rings reported earlier . An anomalously salty parcel of Mediterranean water in this section is typical of highly saline lenses seen in the Canary Basin.
The Long Term Upper Ocean Study (Lotus)
Author: Richard P. Trask
Publisher:
ISBN:
Category : Hydrography
Languages : en
Pages : 1178
Book Description
OCEANUS cruise number 129 (28 October - 4 November, 1982) was the eighth in a series of cruises to the Long Term Upper Ocean Study (LOTUS) area centered at 34 deg. N, 70 deg. W. In the LOTUS area seven SOFAR floats were launched, two moorings were recovered (a LOTUS surface mooring and a C.S. Draper Labs profiling current meter mooring), and a surface mooring which replaced the one recovered was set. Seven CTD stations were also completed in the LOTUS area. Outside the LOTUS area a subsurface mooring was set in the Gulf Stream in cooperation with H. Bryden's (WHOI) Gulf Stream Observations project, and a WHOI engineering mooring at Site D was recovered, examined and redeployed. In addition, several XBT sections were made, one along 70 deg. W between 40 deg. N and 34 deg. N, a second surveyed a cold core ring discovered during the trip to the LOTUS area and a third was made in the vicinity of the Gulf Stream Observations mooring. Part I of this report is a summary of the major cruise activities and part II presents the hydrographic data (CTD and XBT) collected during the cruise. (Author).
Publisher:
ISBN:
Category : Hydrography
Languages : en
Pages : 1178
Book Description
OCEANUS cruise number 129 (28 October - 4 November, 1982) was the eighth in a series of cruises to the Long Term Upper Ocean Study (LOTUS) area centered at 34 deg. N, 70 deg. W. In the LOTUS area seven SOFAR floats were launched, two moorings were recovered (a LOTUS surface mooring and a C.S. Draper Labs profiling current meter mooring), and a surface mooring which replaced the one recovered was set. Seven CTD stations were also completed in the LOTUS area. Outside the LOTUS area a subsurface mooring was set in the Gulf Stream in cooperation with H. Bryden's (WHOI) Gulf Stream Observations project, and a WHOI engineering mooring at Site D was recovered, examined and redeployed. In addition, several XBT sections were made, one along 70 deg. W between 40 deg. N and 34 deg. N, a second surveyed a cold core ring discovered during the trip to the LOTUS area and a third was made in the vicinity of the Gulf Stream Observations mooring. Part I of this report is a summary of the major cruise activities and part II presents the hydrographic data (CTD and XBT) collected during the cruise. (Author).
Hydrographic Data from R. V. Endeavor Cruise 129
Author: George P Knapp
Publisher:
ISBN:
Category : Hydrography
Languages : en
Pages : 692
Book Description
Hydrographic and CTD data collected during R.V. Endeavor cruise 129 are presented. These data include temperature, salinity and dissolved oxygen observed at standard levels by a Neil Brown Instrument Systems' CTD-02 profiler and salinity, dissolved oxygen, silica, phosphate and nitrate values at the observed depths of the collected water samples. Ninety- two stations were occupied on two short sections within the Caribbean and one long meridional section at (nominally) 64° West from the British Virgin Islands to the 200 m depth contour south of Newfoundland. Also presented are a series of sectional profiles of the six observed parameters as a function of depth.
Publisher:
ISBN:
Category : Hydrography
Languages : en
Pages : 692
Book Description
Hydrographic and CTD data collected during R.V. Endeavor cruise 129 are presented. These data include temperature, salinity and dissolved oxygen observed at standard levels by a Neil Brown Instrument Systems' CTD-02 profiler and salinity, dissolved oxygen, silica, phosphate and nitrate values at the observed depths of the collected water samples. Ninety- two stations were occupied on two short sections within the Caribbean and one long meridional section at (nominally) 64° West from the British Virgin Islands to the 200 m depth contour south of Newfoundland. Also presented are a series of sectional profiles of the six observed parameters as a function of depth.
The Long Term Upper Ocean Study (Lotus)
Author: Richard P. Trask
Publisher:
ISBN:
Category : Navigation
Languages : en
Pages : 882
Book Description
OCEANUS cruise number 119 (6-14 May, 1982) was the seventh in a series of cruises to the Long Term Upper Ocean Study (LOTUS) area centered at 34 N, 70 W. During this cruise five moorings were set at the LOTUS site; four for the LOTUS experiment and one, a profiling current meter mooring, for C.S. Draper Labs - MIT. In addition, an engineering mooring was set at 39 deg 30 min N, 70 W. Two XBT sections were made along 70 W between 40 N and 33 N during the trip to and from the LOTUS site. Five CTD stations were also completed in the LOTUS area. Part I of this report is a summary of the major cruise activities and part II presents the hydrographic data (CTD and XBT) collected during the cruise.
Publisher:
ISBN:
Category : Navigation
Languages : en
Pages : 882
Book Description
OCEANUS cruise number 119 (6-14 May, 1982) was the seventh in a series of cruises to the Long Term Upper Ocean Study (LOTUS) area centered at 34 N, 70 W. During this cruise five moorings were set at the LOTUS site; four for the LOTUS experiment and one, a profiling current meter mooring, for C.S. Draper Labs - MIT. In addition, an engineering mooring was set at 39 deg 30 min N, 70 W. Two XBT sections were made along 70 W between 40 N and 33 N during the trip to and from the LOTUS site. Five CTD stations were also completed in the LOTUS area. Part I of this report is a summary of the major cruise activities and part II presents the hydrographic data (CTD and XBT) collected during the cruise.
Hydrographic Data from the First Coastal Ocean Dynamics Experiment
The Subduction Experiment. Cruise Report, R/V Oceanus, Cruise Number 250 Legs 1 and 2. Subduction 2 Mooring Deployment and Recovery Cruise, 25 January-26 February 1992
Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 106
Book Description
Subduction is the mechanism by which water masses formed in the mixed layer and near the surface of the ocean find their way into the upper thermocline. The subduction process and its underlying mechanisms were studied through a combination of Eulerian and Langrangian measurements of velocity, measurements of tracer distributions and hydrographic properties and modeling. An array of five surface moorings carrying meteorological and oceanographic instrumentation were deployed for a period of two years beginning in June 1991 as part of an Office of Naval Research (ONR) funded Subduction experiment. Three eight month deployments were planned. The initial deployment of five surface moorings took place during the third leg of R/V Oceanus cruise number 240. The moorings were deployed at 18 deg N 34 deg W, 18 deg N 22 deg W, 25.5 deg N 29 deg W, 33 deg N 22 deg W and 33 deg N 34 deg W.A Vector Averaging Wind Recorder (VAWR) and an Improved Meteorological Recorder (IMET) collected wind speed and wind direction, sea surface temperature, air temperature, short wave radiation, barometric pressure and relative humidity. The IMET also measured precipitation. The moorings were heavily instrumented below the surface with Vector Measuring Current Meters (VMCM) and single point temperature recorders. Expendable bathythermograph (XBT) data were collected and meteorological observations were made while transitting between mooring locations. This report describes the work that took place during R/V Oceanus cruise 250 which was the second scheduled Subduction mooring cruise. During this cruise the first setting of the moorings were recovered and redeployed for a second eight month period ... Air-sea interaction, Moored instruments, Subduction.
Publisher:
ISBN:
Category :
Languages : en
Pages : 106
Book Description
Subduction is the mechanism by which water masses formed in the mixed layer and near the surface of the ocean find their way into the upper thermocline. The subduction process and its underlying mechanisms were studied through a combination of Eulerian and Langrangian measurements of velocity, measurements of tracer distributions and hydrographic properties and modeling. An array of five surface moorings carrying meteorological and oceanographic instrumentation were deployed for a period of two years beginning in June 1991 as part of an Office of Naval Research (ONR) funded Subduction experiment. Three eight month deployments were planned. The initial deployment of five surface moorings took place during the third leg of R/V Oceanus cruise number 240. The moorings were deployed at 18 deg N 34 deg W, 18 deg N 22 deg W, 25.5 deg N 29 deg W, 33 deg N 22 deg W and 33 deg N 34 deg W.A Vector Averaging Wind Recorder (VAWR) and an Improved Meteorological Recorder (IMET) collected wind speed and wind direction, sea surface temperature, air temperature, short wave radiation, barometric pressure and relative humidity. The IMET also measured precipitation. The moorings were heavily instrumented below the surface with Vector Measuring Current Meters (VMCM) and single point temperature recorders. Expendable bathythermograph (XBT) data were collected and meteorological observations were made while transitting between mooring locations. This report describes the work that took place during R/V Oceanus cruise 250 which was the second scheduled Subduction mooring cruise. During this cruise the first setting of the moorings were recovered and redeployed for a second eight month period ... Air-sea interaction, Moored instruments, Subduction.