goos/gcos measurements of near-surface currents

GOOS/GCOS measurements of near-surface currents

GOOS/GCOS measurements of near-surface currents

Rick LumpkinRick Lumpkin([email protected])([email protected])

National Oceanic and Atmospheric Administration (NOAA)Atlantic Oceanographic and Meteorological Laboratory (AOML)

Miami, Florida USA

Silvia Garzoli and Gustavo GoniSilvia Garzoli and Gustavo GoniNOAA/AOML

Peter NiilerPeter NiilerNOAA/JIMO

Office of Climate Observations 6th Annual System Review, 3 September 2008

Drifters + altimetry in the South Atlantic

Shading: SSTA trend, 1993—2002 (C) from NCEP/NCAR.v2 reanalysis.

Brazil-Malvinas Confluence

Lumpkin & Garzoli (2008)


Latitude of the Brazil-Malvinas Confluence

Trend: 0.860.06 degrees per decade


-1.060.56 degrees per decade

Lat

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Assessment of the global observing array

Analogy with SST analysis:Potential Satellite Bias Error

Satellite measurements Model Field at surface

Biases in model: biases in resulting field.

In-situ observations: reduce bias.

Resulting bias error is a function of observing system configuration and biases in various platforms.

Near-surface currentsWhat model converts satellite measurements to near-surface currents?

OSCAR: the most mature satellite-based surface current product.

Web page offers comparisons with moored and drifting buoys in various regions.

However, the OSCAR currents aren’t accompanied by formal error bars needed to asses bias.

Drifter motion:

.residslipgeoEk uuuuu

Five-day lowpass: filter tides, inertial oscillations, submesoscale.

GOAL: forecast surface velocities (and drifter trajectories) with wind and altimetry products, including error bars.

Assess Potential Satellite Bias Error.


Ekman: Ralph and Niiler (1999), Niiler (2001).

Geostrophic mean from hydrographic climatology, variations addressed by averaging in 2° 5° bins.

./ fAuEk Mean angle 54° off the wind.

For NCEP winds, best fit A=0.081 s-1/2.


Geostrophic: For many studies (e.g., Rio and Hernandez, 2003),

,'SLAgeo uuu .

''

f

guSLA

Left: Altimeter EKE minus drifter EKE (Fratantoni, 2001).

Several reasons that these can differ in general, even if Ekman and slip are perfectly removed:

• centrifugal force, submesoscale motion, etc.

• mismatch between spatial smoothing of altimetry, temporal smoothing of drifters, and energy spectra of motion.


Niiler et al., (2003): .)( 'SLACgeo uxGuu

Drifter measurements

Drifter mean (biased)

Unbiased mean

SLA geo.vel.anomaly

G(x)

Absolute sea level height (cm) (from Niiler, Maximenko & McWilliams, 2003)


Niiler et al., (1995), Niiler and Paduan (1995):

Pazan and Niiler (2001): uundrogued=udrogued+(7.910-3)W.

.WR

Auslip

Drag area ratio

Best fit: A=0.07

Wind speed

Holey-sock drifters: R=40.

Slip is 1.8 cm/s in 10 m/s wind.

Slip in high wind/wave stateNiiler et al. (1995) measurements of slip were in W8 m/s.

Slip may exceeds linear relationship at high wind/wave state.

Niiler, Maximenko and McWilliams (2003): absolute sea height change, 40—60°S: 2.34m, all drifters; 1.98m, only drifters in W8 m/s; 1.55 m, hydrography referenced to floats (Gille, 2003).

Discrepancies with models: problems with models or with data?

Left: mean zonal drifter speed (AOML climatology) minus mean zonal speed of ECCO-GODAE 1° state estimation, 15yr mean (figure courtesy M. Mazloff, WHOI).

Consistent offset in Southern Ocean.

How we can improve our understanding of drifter motion?

• Use high resolution scatterometer-based wind product and include ocean currents when calculating wind stress.

• Simultaneously project motion into geostrophic, wind-driven, and residual components.

slipMDT uuu

./)ˆˆ(ˆˆ)1( 5432'

1 nτu jxixjxixx av

Solve in bins using Gauss-Markov estimation.

(Lumpkin and Elipot, in preparation)

Wind and wind stress

Winds: 6 h, 25 km resolution Variational Analysis Method (VAM) product (Atlas et al., 1996; Atlas et al., 2008) derived from SSM/I, AMSR-E, TMI, QuickSCAT, SeaWinds, and in-situ observations and ECMWF analysis.

Stress: Smith (1988) algorithm as implemented in COARE 3.0 (Fairall et al., 2003) applied to VAM wind and drifter downwind speed (if drifter speed=wind speed, stress=0).

A priori errors 2/Rf

gu

Results

Globally-averaged gain: 1.13±0.06

Gain coefficient (shading) and time-mean currents (arrows)

Wind-driven motion

Comparison with Ralph & Niiler (1999)./ fAuEk .//* AfH

Where do these results differ from RN99?

Where do these results differ from RN99?

.1 32ag

U s a: using significant wave height.

: using peak wave period.

Difference vs. wind, waves

Residuals

Potential Satellite Bias Error (globally averaged)

SummaryWithin assumed error, 5d lowpassed drifter velocities can be estimated as sum of geostrophic and wind-driven. Residual has structure related to EKE maxima.

AVISO altimetry generally underestimates observed EKE, presumably due to smoothing in OI. But some regions are overestimated with a gain of 1. Ageostrophic terms in surface momentum budget.

Wind-driven component is consistent with Ralph and Niiler (1999) in much of the tropics, subtropics. However, high wind areas have larger downwind motion. The spatial variations in the wind-driven part may be due to Stokes drift in wave field. This will be included explicitly in the next version of the model.

Stokes drift: 10—20 cm/s increase in time-mean, in some regions of the Southern Ocean.

goos/gcos measurements of near-surface currents

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