Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker,...

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Aquarius optimum Aquarius optimum interpolation analysis for interpolation analysis for global and regional studies global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D Science Team Meeting 11-14 November 2014, Seattle, Washington 76x94 km 84x120 km 96x156 km 3 beams 390 km wide swath

Transcript of Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker,...

Page 1: Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D.

Aquarius optimum interpolation Aquarius optimum interpolation analysis for global and regional studiesanalysis for global and regional studies

O. Melnichenko, P. Hacker, N. Maximenko, G. O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. PotemraLagerloef, and J. Potemra

2014 Aquarius/SAC-D Science Team Meeting

11-14 November 2014, Seattle, Washington

76x94 km

84x120 km96x156 km

3 beams 390 km wide swath

Page 2: Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D.

Objectives:Objectives: To develop gridded SSS analysis from Aquarius Level 2 (swath) data and improve the utility (reduce the noise) of the SSS fields:

1) Near-global coverage

2) From Sep 2011 - present

3) (O~150 km) spatial scales

4) Weekly temporal scales

5) Global RMS error < 0.2 psu

Challenges:Challenges: satellite biases, high level of instrument noise; correlated errors

Approach:Approach: 1) correction for large-scale biases, 2) optimum interpolation (OI) that takes into account analyzed errors on the observations, specific to the Aquarius instrument

Page 3: Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D.

Beam 2 Beam 2

Beam 3 Beam 3

Beam 1 Beam 1

Ascending Descending

Mean spatial bias correction fields for Aquarius ascending (left) and descending (right) data and for each of the three beams.

Correction for large-scale satellite biases: SSS obsadj

Page 4: Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D.

Input information for OIInput data: Aquarius along-track SSS smoothed with a running Hanning filter of half-width of ~60 km.

Latitude

SS

S

Signal covariance: from Aquarius L2 data

)/exp()( 22 Rrrc

R,

km

Latitude

AquariusOI model

R92 106 km

First guess: Argo-derived monthly SSS (IPRC product)

Example: September 2011

Long-wavelength error covariance:

Statistics of the inter-beam biases are inferred from Aquarius – HYCOM inter-comparison.

)/exp()( llong Rllc lR =500 km

wijji

longwijji x

Error covariance matrix (Le Traon et al., 1998):

Melnichenko et al. [2014], JAOTec, 31, 1583-1600

Page 5: Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D.

Sep 3-9, 2011

Sub-Arctic Front in the North Pacific Amazon River Plume

Sep 9-15, 2012

Far Eastern Pacific Fresh Pool

Feb 12-18, 2012

A new gridded SSS product from Aquarius

The Aquarius OI SSS dataset is open for The Aquarius OI SSS dataset is open for free unrestricted use and can be accessed free unrestricted use and can be accessed from the APDRC webpage: from the APDRC webpage:

http://apdrc.soest.hawaii.edu/datadoc/oisss.php

Page 6: Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D.

Argo SSS September 2011 (first guess) Aquarius OI SSS September 2011

grad(SSS) grad(SSS)

psu

/10

0km

A new high-resolution SSS product from Aquarius

Page 7: Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D.

The error statistics are calculated by comparing Argo buoy measurements for a given week (~1000, z < 6 m) with SSS values at the same locations obtained by interpolating the corresponding Aquarius-derived SSS maps.

Statistics of the differences between Argo buoy data and Aquarius OI SSS analysis for the period from September 2011 through August 2014

Mea

n D

iffer

ence

, ps

uR

MS

D,

psu

OI SSS

L3 bias_adj

L3 original

Page 8: Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D.

Latitude-time distributions of the zonally averaged differences between weekly SSS maps and the corresponding Argo buoy data

(a) Standard Level-3 product without bias correction, (b) Standard Level-3 product with SST-dependent bias correction, and (c) OI SSS

OI SSSL3 bias_adjL3 original

Page 9: Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D.

RMS Differences (psu) between weekly OI SSS maps and concurrent Argo buoy data

Sampling RMS error due to unresolved small-scale variability from Vinogradova and Ponte [2013]

0 0.02 0.04 0.06 0.08 0.1 0.12 0.14 0.16 0.18 0.2

Sampling RMS Error

Differences can be due to

1. Misrepresentation of SSS by buoy measurements at 5 m depth

2. Unresolved small-scale variability

3. Unresolved temporal variability

4. Errors in the SSS maps

5. All of the above

Statistics of the differences between Argo buoy data and Aquarius OI SSS analysis for the period from September 2011 through August 2014

Page 10: Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D.

ConclusionsConclusions

The Aquarius OI SSS analysis can be assessed from the APDRC webpage http://apdrc.soest.hawaii.edu/datadoc/oisss.php either through the Live Access Server or OPeNDAP.

The description of the mapping methodology as well as some results on statistical validation of the product against concurrent in-situ data can be found in the Technical Notes: http://iprc.soest.hawaii.edu/users/oleg/oisss/glb/Technical_Notes.pdf

We hope that you find the data useful. Please send comments/questions to [email protected].

Page 11: Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D.

Long-wavelength error correction is switched off

OI SSS analysis for the week September 10-16, 2011

Long-wavelength error correction is switched on

longwijji

longwijji

Page 12: Aquarius optimum interpolation analysis for global and regional studies O. Melnichenko, P. Hacker, N. Maximenko, G. Lagerloef, and J. Potemra 2014 Aquarius/SAC-D.

Aquarius – Met Office

Aquarius – Met Office

Aquarius - APDRC

Aquarius - APDRC

Static bias (3-year mean)

AscendingAscending

DescendingDescending