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Ocean Surface Topography from Space
SCIENCE
Barotropic high-frequency sea level signals and the Jason-1 altimeter mission

Figure1

Authors:


R.M. Ponte
(AER Inc., USA)

CORRESPONDING AUTHOR:
Rui Ponte
Atmospheric and Environmental Research, Inc.
131 Hartwell Avenue
Lexington, MA 02421-3216
ponte@aer.com


SIZE="2">

Abstract:

Atmospheric surface fields, particularly winds and pressure, drive significant sea level variability at frequencies not
well-resolved by the Jason-1 altimeter sampling. Such rapid signals can thus hamper the interpretation of the altimeter
records. Our Jason-1 investigation focuses on determining the sea level response to high-frequency atmospheric forcing
using a combination of numerical modeling, data analysis, and state estimation techniques. Efforts will lead to improved
knowledge of rapid sea level signals, their dynamics and relation to atmospheric forcing, and to estimates of such signals
that can be used to improve the processing and analysis of altimeter observations and extend their range of applications.

Content:

With its repeat cycle of about 10 days, Jason-1 will poorly resolve sea level (zeda)
signals at periods shorter than about 20 days. Analyses of in situ tide gauge and bottom pressure data show a substantial amount
of variance over these time scales. Recent model results and comparisons with data indicate that wind-forced high
frequency (HF) signals can be a source of large aliasing in the altimeter records, particularly at mid and high latitudes.
Signals forced by pressure (pa) can also add to the problem. In particular, the HF zeda response to pa does not follow the
"inverted barometer" (IB) model; the isostatic zeda adjustment to pa at a rate of approximately -1 cm/hPa that holds at
longer time scales. Our general goal is to move closer to a full determination of the atmospherically-forced HF zeda signals
and a better understanding of their dynamics and relation to forcing. The focus is on signals driven by surface winds and
pa. By improving current knowledge of these atmospheric forcing fields and by developing the necessary modeling and
optimization tools, we seek to estimate the HF zeda signals as best as possible. Such estimates should provide for the
removal of some of the HF noise in the Jason-1 records, leading to cleaner data products that can benefit the general
altimeter user.

To arrive at useful estimates of the HF zeda signals, one needs to know well the relevant
atmospheric forcing fields and their error statistics. In this regard, comparisons among the different forcing
products provided by various weather centers are useful (figure 1). Our assessment of the forcing fields also
involves comparisons with independent data (e.g., island pressure stations) and combined analysis with altimeter
data (e.g., checking the effects of IB corrections based on different pa fields). Improved representation of the
forcing fields can lead directly to improved altimeter data processing (e.g., better pa fields yield better
environmental corrections), as well as to better estimates of HF zeda signals obtained from combined model and data
analysis.


Figure 2

Given the HF and large scales of interest, modeling work focuses on the use of simple barotropic (constant density) models.
Modeling efforts include an evaluation of effects of different forcing fields on the sea level response, assessment of
sensitivity of results to different parameterizations of bottom friction, and implementation of increasingly smaller
grid spacing to improve the representation of coastal geometry and bottom topography (figure 2). Comparisons of different
numerical models are intended to check for inconsistencies and learn about the various factors affecting the realism of
the numerical solutions.

Straightforward model comparisons with data (mostly altimeter but also tide gauge) should provide a measure of their
consistency and lead to model improvements. Ultimately, the goal of achieving an "optimal" estimate of HF zeda signals
related to atmospheric forcing is best approached through estimation schemes that combine model and data in an optimal
fashion. Part of our investigation is devoted to the development of assimilation techniques that combine barotropic
models and altimeter data to provide dynamically-based estimation of atmospherically-driven signals over the global
ocean. Such estimates of HF zeda signals can be used to "correct" the altimeter data, just as tide models are currently
applied to remove the large HF tidal signals from the records. Sorting out the variability in the records due to HF
winds and pa forcing will allow a better analysis of other less understood components.

In addition, analyses of the model results and estimated HF zeda fields carried out during our investigation will shed
light on many scientific issues of current importance in oceanography. Specific topics of study include: the validity
of the IB approximation as a function of location and time; the relative importance of winds and pa as forcing mechanisms
for HF oceanic variability; the relevant dissipation mechanisms for HF barotropic motions in the ocean and appropriate
ways of parameterizing such processes in numerical models; and the influence of topography on HF dynamics. In summary,
our efforts will lead to significant improvements in current understanding of the sea-level response to HF atmospheric
forcing, while providing for more precise analysis and interpretation of the altimeter signals and moving us closer to
meeting the 1-cm accuracy challenge for Jason-1.

References

N. Hirose, I. Fukumori, V. Zlotnicki, R.M. Ponte, 2001: High-frequency barotropic response to atmospheric disturbances: Sensitivity to forcing, topography, and friction. J. Geophys. Res. (submitted).


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