Featured Publications

How Does Our Ocean "Pass the Salt"? Ask ECCO

Time evolution of globally averaged deep ocean salinity
Time evolution of globally averaged deep ocean salinity calculated as deviations from the temporal means from January 1993 to December 2014. Credit: Liu et al., 2019, Fig. 1b; image modified from open-source article.
Time evolution of globally averaged deep ocean salinity
Time evolution of globally averaged deep ocean salinity calculated as deviations from the temporal means from January 1993 to December 2014. Credit: Liu et al., 2019, Fig. 1b; image modified from open-source article.
Liu, C., Liang, X., Ponte, R., Vinogradova, N., and Wang, O. (2019). Vertical Redistribution of Salt and Layered Changes in Global Ocean Salinity, Nat. Commun., 10, 3445, doi: 10.1038/s41467-019-11436-x.
When compared to the variable flux of freshwater at the ocean's surface, the amount of dissolved salt in our ocean basins is relatively stable. Thus, understanding changes in salinity is key to estimating the global net freshwater input into our ocean. Moreover, processes related to climate warming ­- such as ocean freshening from the melting of glaciers and ice sheets, and salt rejection during sea ice formation - have affected the vertical distribution of salt of in our seas.
To understand these types of connections, salinity and related dynamical processes must be reliably represented, both globally and over the ocean's full depth. So, investigators have used ECCO global state estimates, in which salt and heat budgets are explicitly closed, to examine how salinity has changed over two decades.
Horizontally averaged, the salt budget reveals trends within distinct ocean layers: some depths have freshened over time while others have become saltier. The study also focuses on the vertical redistribution of salt in the upper mile of the ocean, within the range of Argo profiling floats. These salt transport processes are parsed among ocean motion (e.g., currents and eddies), diffusion, and brine rejection, and knowing them permits more robust inferences about surface freshwater fluxes from observed salinity changes. Study results also reveal regional patterns including the essential role of vertical salt fluxes at high latitudes. MORE »

ECCO Helps Debunk the "Ocean Conveyor Belt"

Forget, G. and Ferreira, D. (2019). Global Ocean Heat Transport Dominated by Heat Export from the Tropical Pacific, Nat, Geosci., 12, 351-354, doi: 10.1038/s41561-019-0333-7.
Earth's climate is regulated by the exchange and storage of heat between the ocean and the atmosphere. Thus, it is important to understand the pathways of ocean heat. This includes distinguishing between heat that is exchanged with our atmosphere - potentially warming our climate - and heat that merely circulates within our ocean. Investigators have used ECCO's state-of-the-art, global gridded data product to provide a new perspective on ocean heat transport. MORE »

Using ECCO Estimates for Studies in Geodesy

Quinn, K.J., Ponte, R.M, Heimbach, P., Fukumori, I., and Campin, J.-M., (2018). Ocean Angular Momentum from a Recent Global State Estimate, with Assessment of Uncertainties, Geophys. J. Int., 216(1), 584-597, doi: 10.1093/gji/ggy452.
The ocean is a key factor in determining and understanding the geodetic properties of the Earth. For example, changes in the oceanic mass field can have important effects on crustal loading. Knowledge of the mean ocean surface circulation and dynamic topography can help determine the marine geoid and the gravity field. And variability in both ocean currents and bottom pressure can affect the Earth's orientation in space. MORE »

A New 20-year Ocean Climatology

Fukumori, I., Heimbach, P., Ponte, R.M., and Wunsch, C. (2018). A Dynamically Consistent, Multivariable Ocean Climatology, Bull. Am. Meteorol. Soc., 99, 2107-2128, doi: 10.1175/BAMS-D-17-0213.1.
A new 20-year ocean climatology has been created for ocean circulation and climate studies based on the recent ECCO Version 4 release 3 ocean state estimate. In comparison to conventional climatologies based on observations alone, the new ECCO climatology accounts for the very great inhomogeneity with which the ocean has been observed. MORE »

Ocean-induced Melt Triggers Glacier Retreat in Northwest Greenland

Wood, M., Rignot, E., Fenty, I., Menemenlis, D., Millan, R., Morlighem, M., Mouginot, J. & Seroussi, H. (2018). Ocean-induced Melt Triggers Glacier Retreat in Northwest Greenland, Geophys. Res. Lett., 45(16), 8334-8342. doi: 10.1029/2018GL078024.
In recent decades, tidewater glaciers in Northwest Greenland have contributed significantly to sea level rise but have also exhibited a complex spatial pattern of retreat that remained unexplained. In this new study, NASA's Oceans Melting Greenland (OMG) data are used in combination with ECCO model outputs to assess the role of the ocean in triggering the retreat of these glaciers. MORE »

Mechanisms of the Recent Decadal Trend of the North Atlantic Ocean Heat Content

Piecuch, C.G., Ponte, R.M., Little, C.M., Buckley, M.W., and Fukumori, I. (2017). Mechanisms Underlying Recent Decadal Changes in Subpolar North Atlantic Ocean Heat Content, Geophys. Res. Oceans, 122(9), 7181-7197, doi: 10.1002/2017JC012845.
The subpolar North Atlantic (SPNA) reversed trends in ocean heat content from warming during 1994-2004 to cooling over 2005-2015. ECCO V4r3 reveals that this reversal is the result of anomalous horizontal midlatitude gyre circulation acting on the mean temperature gradient, rather than changes in overturning circulation. Results have implications for decadal predictability. MORE »

Coherent Arctic Ocean Bottom Pressure Variations

Fukumori, I., Wang, O., Llovel, W., Fenty, I., and Forget, G. (2015). A Near-uniform Fluctuation of Ocean Bottom Pressure and Sea Level Across the Deep Ocean Basins of the Arctic Ocean and the Nordic Seas, Prog. Oceanogr., 134, 152-172, doi: 10.1016/j.pocean.2015.01.013.
Across the Arctic Ocean and the Nordic Seas, GRACE and in-situ observations identified a basin-wide mode of ocean bottom pressure and sea-level fluctuation with spatially near-uniform amplitude and phase. This basin-wide fluctuation is barotropic and dominates the region's large-scale variability from sub-monthly to interannual timescales. MORE »