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www.go-ship.org
GO-SHIP: 2012-2023 Decadal Survey
Introduction
The Global Ocean Ship-based Hydrographic Investigations
Program (GO-SHIP) brings together scientists with
interests in physical oceanography, the carbon cycle,
marine biogeochemistry and ecosystems, and other users
and collectors of ocean interior data to develop a
sustained global network of hydrographic sections as part
of the Global Ocean / Climate Observing System.
GO-SHIP is part of the Global Climate Observing System/ Global
Ocean Observing System GCOS/ GOOS.
GO-SHIP Reference Sections.
GO-SHIP: Program Aims
• Document the large-scale ocean water property
distributions, their changes, and drivers of those
changes
• Determine the distributions and controls of natural
and anthropogenic carbon (both organic and
inorganic),
• Determine ocean ventilation and circulation
pathways and variability using chemical tracers,
• Provide high-quality full-depth reference
observations to other components of the observing
systems.
GO-SHIP Committee
Project Coordinator: Martin Kramp (JCOMMOPS, IOC-UNESCO)
We welcome National Representatives from other nations with an interest
in the decadal global survey
Measurements: Level 1
Measurement: Level 2
Level 2 data
• Discrete pCO2
• 14
C (by AMS)
• CCl4
• ∂13
C of DIC
• Dissolved organic carbon
• Dissolved organic nitrogen
• Fe/trace metals
• CTD Transmissometer
• Surface underway system (nutrients, O2, Chl, skin temperature).
GO-SHIP: Measurements
• Level 1 data are of highest priority. GO-SHIP recommends that
level 1 data should be collect at least once per decade on all
sections. Sections occupied at higher frequencies (yearly,
biennial) do not need to undertake all level 1 measurement on all
re-occupations.
• Level 2 data are highly desirable. GO-SHIP recommends that
level 2 should be collected when possible.
• Level 3 data are ancillary measurements are done according to
opportunity and space available. They should not significantly
interfere with Level 1 or 2 data collection, and may be regional or
specific to an individual cruise.
GO-SHIP Measurement Reference Manual
http://www.go-ship.org/HydroMan.html
Typical Sample Strategy for discrete
Bottle measurements
Deep Ocean Heat Fluxes
Mean local heat fluxes through 4000 m implied by abyssal warming
below 4000 m from the 1990s to the 2000s (from Purkey and Johnson
2010).
Deep Ocean contribution to Sea Level
Rise
Basin means of sea level rise from the 1990s to the 2000s due to abyssal
thermal expansion below 4000 m and deep thermal expansion in the
Southern Ocean from 1000 to 4000 m south of the Subantarctic Front
(from Purkey and Johnson, 2010)
Ocean Mixing Spatial Variability
Diapycnal diffusivity κ along 32°S in the Indian Ocean, estimated from CTD and
LADCP profiles (Kunze et al. 2006) using a finescale parameterization,
representative of numerous recent studies (e.g., Polzin et al. 2014).
Anthropogenic Carbon Storage
GO-SHIP/
GLODAP
IOCCP/
SOCAT
Air-sea CO2 Flux
anthropogenic CO2
storage
Decadal Anthropogenic Carbon Storage Rate
Decadal storage rates of anthropogenic carbon (mol m-2
yr-1
), as observed from
repeat hydrography cruises. (Upper panels): The horizontal lines depict the
measurement intervals bracketed by repeat hydrography cruises. Lower panels):
Maps of decadal storage rates from a Green’s function inversion averaged over 1980-
2005 using data shown in top panels. (From Khatiwala et al. 2013.)
GO-SHIP: Global Decadal Survey
The GO-SHIP web site has information on planned occupation dates
GO-SHIP: Global Decadal Survey
The GO-SHIP web site has information on planned occupation dates
GO-SHIP: Contacts
Bernadette Sloyan (GO-SHIP Co-Chair):
Bernadette.Sloyan@csiro.au
Rik Wanninkhof (GO-SHIP Co-Chair):
rik.wanninkhof@noaa.gov
Martin Kramp ( GO-SHIP Project
Coordinator):
mkramp@jcommops.org
C5.04: GO-SHIP: A component of the sustained ocean observing system - Bernadette Sloyan

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C5.04: GO-SHIP: A component of the sustained ocean observing system - Bernadette Sloyan

  • 2. Introduction The Global Ocean Ship-based Hydrographic Investigations Program (GO-SHIP) brings together scientists with interests in physical oceanography, the carbon cycle, marine biogeochemistry and ecosystems, and other users and collectors of ocean interior data to develop a sustained global network of hydrographic sections as part of the Global Ocean / Climate Observing System. GO-SHIP is part of the Global Climate Observing System/ Global Ocean Observing System GCOS/ GOOS.
  • 4. GO-SHIP: Program Aims • Document the large-scale ocean water property distributions, their changes, and drivers of those changes • Determine the distributions and controls of natural and anthropogenic carbon (both organic and inorganic), • Determine ocean ventilation and circulation pathways and variability using chemical tracers, • Provide high-quality full-depth reference observations to other components of the observing systems.
  • 5. GO-SHIP Committee Project Coordinator: Martin Kramp (JCOMMOPS, IOC-UNESCO) We welcome National Representatives from other nations with an interest in the decadal global survey
  • 7. Measurement: Level 2 Level 2 data • Discrete pCO2 • 14 C (by AMS) • CCl4 • ∂13 C of DIC • Dissolved organic carbon • Dissolved organic nitrogen • Fe/trace metals • CTD Transmissometer • Surface underway system (nutrients, O2, Chl, skin temperature).
  • 8. GO-SHIP: Measurements • Level 1 data are of highest priority. GO-SHIP recommends that level 1 data should be collect at least once per decade on all sections. Sections occupied at higher frequencies (yearly, biennial) do not need to undertake all level 1 measurement on all re-occupations. • Level 2 data are highly desirable. GO-SHIP recommends that level 2 should be collected when possible. • Level 3 data are ancillary measurements are done according to opportunity and space available. They should not significantly interfere with Level 1 or 2 data collection, and may be regional or specific to an individual cruise.
  • 9. GO-SHIP Measurement Reference Manual http://www.go-ship.org/HydroMan.html
  • 10. Typical Sample Strategy for discrete Bottle measurements
  • 11. Deep Ocean Heat Fluxes Mean local heat fluxes through 4000 m implied by abyssal warming below 4000 m from the 1990s to the 2000s (from Purkey and Johnson 2010).
  • 12. Deep Ocean contribution to Sea Level Rise Basin means of sea level rise from the 1990s to the 2000s due to abyssal thermal expansion below 4000 m and deep thermal expansion in the Southern Ocean from 1000 to 4000 m south of the Subantarctic Front (from Purkey and Johnson, 2010)
  • 13. Ocean Mixing Spatial Variability Diapycnal diffusivity κ along 32°S in the Indian Ocean, estimated from CTD and LADCP profiles (Kunze et al. 2006) using a finescale parameterization, representative of numerous recent studies (e.g., Polzin et al. 2014).
  • 15. Decadal Anthropogenic Carbon Storage Rate Decadal storage rates of anthropogenic carbon (mol m-2 yr-1 ), as observed from repeat hydrography cruises. (Upper panels): The horizontal lines depict the measurement intervals bracketed by repeat hydrography cruises. Lower panels): Maps of decadal storage rates from a Green’s function inversion averaged over 1980- 2005 using data shown in top panels. (From Khatiwala et al. 2013.)
  • 16. GO-SHIP: Global Decadal Survey The GO-SHIP web site has information on planned occupation dates
  • 17. GO-SHIP: Global Decadal Survey The GO-SHIP web site has information on planned occupation dates
  • 18. GO-SHIP: Contacts Bernadette Sloyan (GO-SHIP Co-Chair): Bernadette.Sloyan@csiro.au Rik Wanninkhof (GO-SHIP Co-Chair): rik.wanninkhof@noaa.gov Martin Kramp ( GO-SHIP Project Coordinator): mkramp@jcommops.org