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The Southern Ocean Observing System SOOS

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Title: The Southern Ocean Observing System SOOS


1
The Southern Ocean Observing System (SOOS)
With additional support from
2
Talk Outline
  • Why are coherent, sustained observations of the
    Southern Ocean needed?
  • Who would use them?
  • What aspects of the Southern Ocean would a
    monitoring system address, and how?
  • What is already in place, and what are the gaps?
  • Where are we in relation to planning and
    implementing the observing system, and what is
    next?
  • How would a SOOS link to other international
    efforts?

3
Talk Outline
  • Why are coherent, sustained observations of the
    Southern Ocean needed?
  • Who would use them?
  • What aspects of the Southern Ocean would a
    monitoring system address, and how?
  • What is already in place, and what are the gaps?
  • Where are we in relation to planning and
    implementing the observing system, and what is
    next?
  • How would a SOOS link to other international
    efforts?

4
Global reach of the Southern Ocean
Lumpkin and Speer (2006)
Critical part of the global thermohaline
circulation
5
Change in zonally-integrated ocean heat content
since 1955 is largest in the southern oceans
Levitus et al., 2005
Important term in global heat budget, but
Southern Ocean is still undersampled compared
with rest of World Ocean
6
Ocean uptake of carbon dioxide
Sabine et al., 2004
Southern Ocean a key region for uptake of
anthropogenic CO2 but is the carbon sink
weakening (Le Quéré etc)?
7
Why a SOOS (continued) ?
  • Krill stocks in key parts of the Southern Ocean
    are in steep decline need to understand why, and
    the implications.

(Atkinson et al., Nature, 2004)
8
Warming in ACC, no change in overturning?
Comparison of Argo CTD data along streamlines
shows warming across the Southern Ocean,
strongest on southern flank of ACC. Southward
shift of isopycnals BUT little change in tilt,
hence no change in upwelling (unlike in IPCC
models).
Boening et al., 2008
9
Freshening of AABW
10
Why a SOOS (continued) ?
  • Changes in Southern Ocean temperature and
    circulation could have strong impacts on West
    Antarctic ice sheet (and hence global sea level)
  • Nutrients exported from the Southern Ocean
    support 75 of oceanic primary production north
    of 30S (Sarmiento et al.)
  • The Southern Ocean includes some of the most
    productive and unique marine ecosystems on Earth
  • etc

11
Why do we care if SO changes?
  • Potential for positive feedbacks influencing
    global climate
  • Sea ice albedo
  • Carbon uptake
  • Thermohaline circulation
  • Sea-level rise
  • Impact of acidification on ecosystems
  • Impact of climate change on ecosystems (warming,
    freshening, ?mixed layer, ?light, ?circulation,
    ?sea ice, ?winds)

12
Talk Outline
  • Why are coherent, sustained observations of the
    Southern Ocean needed?
  • Who would use them?
  • What aspects of the Southern Ocean would a
    monitoring system address, and how?
  • What is already in place, and what are the gaps?
  • Where are we in relation to planning and
    implementing the observing system, and what is
    next?
  • How would a SOOS link to other international
    efforts?

13
Potential users of a SOOS include
  • Research community
  • Resource managers (including CCAMLR etc)
  • Policy makers (when is it time to act? What are
    the consequences of not acting?)
  • IPCC
  • Local planners (sea-level rise)
  • Antarctic tourism
  • Shipping operations
  • Weather and climate forecasters
  • Education
  • Etc.

14
Talk Outline
  • Why are coherent, sustained observations of the
    Southern Ocean needed?
  • Who would use them?
  • What aspects of the Southern Ocean would a
    monitoring system address, and how?
  • What is already in place, and what are the gaps?
  • Where are we in relation to planning and
    implementing the observing system, and what is
    next?
  • How would a SOOS link to other international
    efforts?

15
Scope of the SOOS
  • Space
  • circumpolar
  • Subtropical Front to coast / ice shelf grounding
    line
  • Time
  • days to decades (longer-term proxies from ice and
    sediment cores are critical, but lie outside of
    SOOS)
  • Domain
  • sea surface to sea floor (including bathymetry)
  • ocean sea ice
  • include air-sea flux, not upper atmosphere
  • include sub-ice shelf cavity, not glacial ice
    itself
  • Feasibility/readiness
  • consider READY NOW, 5-10 YEAR VISION and BY 2030
  • consider both MINIMAL and IDEAL

16
Scope of the SOOS
  • Discipline
  • physics (ocean circulation and sea ice)
  • biology and ecology (microbes to whales...)
  • biogeochemistry
  • bathymetry
  • surface meteorology
  • Models Emphasis is on sustained observations,
    but modelling plays a key role in
  • system design
  • interpolation and interpretation of sparse
    observations
  • demonstrating utility of SOOS (eg initialisation
    of climate models)

17
Talk Outline
  • Why are coherent, sustained observations of the
    Southern Ocean needed?
  • Who would use them?
  • What aspects of the Southern Ocean would a
    monitoring system address, and how?
  • What is already in place, and what are the gaps?
  • Where are we in relation to planning and
    implementing the observing system, and what is
    next?
  • How would a SOOS link to other international
    efforts?

18
Some examples of observing system elements
already in place
19
Hydrography CTD/XBT/CO2 5-10 yr interval
20
Argo
http//argo.ocean.fsu.edu/
21
Sound sources deployed in Weddell Sea to track
modified Argo floats under ice
22
Tagging of marine mammals (SEaOS etc)
23
Near circumpolar coverage from elephant seal data

Other species can be targeted to access specific
icy regions. Invaluable data for both ecological
and physical sciences.
24
Continuous Plankton Recorder Tows 1991-2008
The Survey coversgt70 of the Southern
Ocean October to April
Approximately40-50 tows each year gt4,000 samples
p.a. 5 n-mile resolution
135,000 nauticalmiles of data havebeen
collected since 1991
This represents morethan 27,000 samples, 200
taxa environmental data
Australia, Japan, NZ, Germany, UK, USA, Russia
Hosie et al
25
  • Above plus-
  • Satellites (e.g. SeaWiFS, Cryosat)
  • Current meter arrays
  • Tide gauge network
  • Sediment trap moorings
  • Underway measurements (e.g. CO2 , Salinity)
  • Sea ice thickness snow cover drift
  • Etc.

What observing system elements are already in
place?
26
Gaps in the observing system in the Southern
Ocean region
  • Ice-covered regions still poorly sampled, despite
    progress
  • Deep ocean below depth of Argo
  • Ocean in ice shelf cavities
  • Seabed is poorly observed (e.g. benthic
    communities)
  • Non-physical measurements rarely routinely made
    (need other sensors for Argo etc.)
  • Etc.

27
Gaps in the observing system in the Southern
Ocean region
  • Routine measurements beneath the ice shelves
    required to understand how the ocean/ice-shelf
    interaction will change as the climate alters,
    and what the impacts may be for deep and bottom
    water formation and the global overturning in the
    ocean
  • Development of new sensors and methodologies is
    key (e.g. biogeochemistry sensors to Argo floats,
    automated under-ice measuring systems, technology
    to study the long-term impact of seasonal ice
    cover on pelagic and benthic communities)

28
Gaps in the observing system in the Southern
Ocean region
  • Need to sample the polar oceans routinely and
    cost-effectively with an appropriate level of
    coverage to capture the main oceanographic,
    meteorological, cryospheric and ecosystems
    processes taking place there that contribute to
    global change

29
Talk Outline
  • Why are coherent, sustained observations of the
    Southern Ocean needed?
  • Who would use them?
  • What aspects of the Southern Ocean would a
    monitoring system address, and how?
  • What is already in place, and what are the gaps?
  • Where are we in relation to planning and
    implementing the observing system, and what is
    next?
  • How would a SOOS link to other international
    efforts?

30
SOOS Timeline
  • August 2006 Initial scoping workshop, Hobart
  • October 2007 Workshop in Bremen. Planning and
    writing tasks assigned
  • July 2008 St. Petersburg progress review meeting
  • April 2009 Make draft SOOS planning document
    available to community for comment
  • May 2009 Comments received
  • June 2009 Publish report
  • July 2009 Commence implementation...

31
SOOS Structure
  • SOOS planning document (to go out to the
    community for comment) will outline the aspects
    discussed here-
  • why sustained observations are needed in the
    Southern Ocean and what science/policy questions
    they address,
  • what mix of observations are required to address
    these questions,
  • what is presently done and what is possible,
  • a vision for the future (in 5-10 years and by
    2030)

32
SOOS designed to address six key challenges
  • Role of Southern Ocean in global freshwater
    balance
  • Stability of Southern Ocean overturning
  • Stability of Antarctic ice sheet and future
    contribution to sea-level rise
  • Future of Southern Ocean carbon uptake
  • Future of Antarctic sea ice
  • Impacts of climate change on Antarctic ecosystems

33
(draft)
34
(draft)
35
Strawman Southern Ocean Observing System
  • Initial SOOS consists of coordination/enhancement
    of extant elements, as discussed, including-
  • Repeat full-depth hydro/tracer sections along
    WOCE lines
  • Profiling floats, open ocean and under sea ice
  • Sensors on marine mammals
  • Sea ice observations
  • Ocean-ice shelf interaction
  • Surface meteorology observations
  • Surface and sea-ice drifters
  • Ecological monitoring

36
Strawman Southern Ocean Observing System
  • 5-10 years and 2030 vision (see planning
    document for details) as previous, but including
  • Enhanced profiling floats with additional
    sensors, depth range and longevity.
  • Cost-effective time series stations, using data
    capsule technology and expendable moorings.
  • Supply/research ships doing routine
    surveys/sections on way into Antarctic bases
  • Network of integrated fast ice mass balance
    stations
  • A network of ice-capable gliders
  • etc

37
Strawman Southern Ocean Observing System
  • SOOS coordination group to oversee the
    implementation of the observing system, plus-
  • Relevant data archaeology
  • Delivery of Southern Ocean climate information
  • Modeling
  • Identification of remote sensing needs
  • Identification of key gaps requiring enhanced
    process understanding
  • Array design studies
  • Technology development requirements

38
Strawman Southern Ocean Observing System
  • As an example recommended repeat hydrography,
    with countries committed or interested in
    occupying the lines.

39
Talk Outline
  • Why are coherent, sustained observations of the
    Southern Ocean needed?
  • Who would use them?
  • What aspects of the Southern Ocean would a
    monitoring system address, and how?
  • What is already in place, and what are the gaps?
  • Where are we in relation to planning and
    implementing the observing system, and what is
    next?
  • How would a SOOS link to other international
    efforts?

40
SOOS Implementation
  • Buy-in of international programmes of relevance
    to SOOS (SCAR, SCOR, GOOS, CAML, POGO,
    WCRP,JCOMM, GCOS...), leading environmental
    agencies and other key players.
  • Links between SOOS, research programmes and
    international organisations will be effected by
    the SOOS coordination group.
  • Group will also oversee coordination of field
    activities development of a funding strategy
    etc.

41
More information
(www.clivar.org/organization/southern/expertgroup/
SOOS.htm)
42
A final word
Many more voyages of discovery are also needed,
especially in the vast expanses of the southern
seas that remain relatively unexplored Trouble
d Waters The Economist, Jan 3rd 2009
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