Observational evidence for propagation of decadal spiciness anomalies in the North Pacific - PowerPoint PPT Presentation

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Observational evidence for propagation of decadal spiciness anomalies in the North Pacific

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Title: Observational evidence for propagation of decadal spiciness anomalies in the North Pacific


1
Observational evidence for propagation of decadal
spiciness anomalies in the North Pacific
  • Yoshi N. Sasaki, N. Schneider, N. Maximenko, and
    K. Lebedev
  • International Pacific Research Center, University
    of Hawaii

2
Subduction of water mass
Qiu and Huang (1995)
  • In the subtropical region, the mixed layer water
    in winter is subducted into the main thermocline
  • Subduction plays an important role in the
    freshwater cycle

3
Decadal salinity variability
Lukas et al. 2008 from the Hawaii Ocean
Time-series (HOT)
PSS-78
  • Spiciness (density compensated) anomaly
  • Sa (x, y,?? ,t) S (x, y,?? ,t) Sclm (x, y,??)
  • warm/salty or cool/fresh
  • passive advection by current
  • Subsurface spiciness signals show substantial
    decadal fluctuations

4
Subduction of spiciness anomaly
?? 25.5 kg m-3
Yeager and Large 2004
  • Several modeling studies showed propagation of
    spiciness signals from the subtropics to the
    equator
  • It is difficult to identify basin-wide
    propagation of spiciness signals from
    observations due to the sparseness of salinity
    observations

5
Argo
  • Argo observations provide a lot of T-S profiles
    with nearly global coverage from the early 2000s
  • ? suitable for examining propagation of spiciness
    signals

6
Purpose
  • To show observational evidence for basin-wide
    propagation of spiciness anomalies in the North
    Pacific
  • propagation speed?
  • decay timescale?

7
Data
  • The Argo profile data are obtained from the US
    Argo Data Assembly Center
  • The each Argo profile is linearly interpolated to
    isopycnal surfaces, and the variables are
    averaged into 3? ? 3? bins for each month
  • We also employ a spatially interpolated dataset
    using the Variational Interpolation algorithm

Number of profiles on 2525.5??
8
Long-term mean on 2525.5??
Montgomery
9
Salinity anomaly
2003
2004
2005
2006
?10 PSS-78
2007
2008
10
Salinity anomaly
2003
2004
2005
2006
?10 PSS-78
2007
2008
11
Salinity anomaly
2003
2004
2005
2006
?10 PSS-78
2007
2008
12
Salinity anomaly
2003
2004
2005
2006
?10 PSS-78
2007
2008
13
Hovmoller diagram
?103 km
?10 PSS-78
14
Trajectory of particles
  • Fifteen parcels are released around the
    cool/fresh spiciness anomaly positions in 2008,
    and their backward trajectories are calculated
    using the mean velocity field

15
Trajectory of particles
16
Trajectory of particles
17
Trajectory of particles
18
Trajectory of particles
19
Trajectory of particles
20
Trajectory of particles
2004
2003
2005
2006
The propagation path and speed show good
agreement with advection by the mean geostrophic
current
2007
2008
21
Hovmoller diagram
?103 km
?10 PSS-78
22
Hovmoller diagram
?103 km
?10 PSS-78
23
Spiciness on streamline coordinate
  • The amplitude of the salinity anomaly of the
    spiciness signal decreases by about 80 from
    -0.15 in 2004 to -0.03 in 2008
  • The anomalies are diffused in the course of
    propagation

24
Summary
  • Argo observations provide an evidence for
    propagation of the spiciness anomalies from the
    eastern subtropics to western tropics
  • The propagation path and speed of the spiciness
    signals are good agreement with advection by the
    mean geostrophic current
  • Sasaki, Y. N., N. Schneider, N. Maximenko and K.
    Lebedev, 2010 Observational evidence for
    propagation of decadal spiciness anomalies in the
    North Pacific. GRL, 37, L07708,
    doi10.1029/2010GL042716.
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