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P D Quay

Biographic Data

ID5601726
NAMEP D Quay
GIVEN NAMESP D
FAMILY NAMEQuay
SIGNATUREQUAY P D
VERIFIEDNo
TOTAL WORKS1
TOTAL CITATIONS3
WORKS AS AUTHOR1
WORKS AS EDITOR0
FIRST PUBLICATION YEAR1980
LATEST PUBLICATION YEAR1980
H-INDEX1
  • Vertical Advection — Diffusion Rates in the Oceanic Thermocline Determined from 14 C Distributions

    Open Access•P D Quay, Minze Stuiver•ARTICLE•Radiocarbon•1980•Cited by: 3•References: 14

    The characteristics of a one-dimensional vertical advection-diffusion ocean mixing model were examined using temperature, salinity, and bomb 14 C measurements made during the GEOSECS program. Vertical advection (W) and eddy diffusion (K) rates for the main oceanic thermocline and CO 2 gas exchange rates (E) were determined from the depth distributions of salinity and bomb produced 14 C measured in the upper 1000m of the Atlantic and Pacific Ocean…

  • Vertical Advection — Diffusion Rates in the Oceanic Thermocline Determined from 14 C Distributions

    Open Access•P D Quay, Minze Stuiver•ARTICLE•Radiocarbon•1980•Cited by: 3•References: 14

    The characteristics of a one-dimensional vertical advection-diffusion ocean mixing model were examined using temperature, salinity, and bomb 14 C measurements made during the GEOSECS program. Vertical advection (W) and eddy diffusion (K) rates for the main oceanic thermocline and CO 2 gas exchange rates (E) were determined from the depth distributions of salinity and bomb produced 14 C measured in the upper 1000m of the Atlantic and Pacific Ocean…

  • Vertical Advection — Diffusion Rates in the Oceanic Thermocline Determined from 14 C Distributions

    Open Access•P D Quay, Minze Stuiver•ARTICLE•Radiocarbon•1980•Cited by: 3•References: 14

    The characteristics of a one-dimensional vertical advection-diffusion ocean mixing model were examined using temperature, salinity, and bomb 14 C measurements made during the GEOSECS program. Vertical advection (W) and eddy diffusion (K) rates for the main oceanic thermocline and CO 2 gas exchange rates (E) were determined from the depth distributions of salinity and bomb produced 14 C measured in the upper 1000m of the Atlantic and Pacific Ocean…

Advection (1 work) · Atmospheric sciences (1 work) · Diffusion (1 work) · Eddy diffusion (1 work) · Geology (1 work) · Geology and Paleoclimatology Research (1 work) · Latitude (1 work) · Marine and coastal ecosystems (1 work) · Meteorology (1 work) · Oceanographic and Atmospheric Processes (1 work)

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