Due to global warming, not only the temperatures in the atmosphere and in the ocean are rising, but also winds and ocean currents as well as the oxygen distribution in the ocean are changing.
Due to global warming, not only the temperatures in the atmosphere and in the ocean are rising, but also winds and ocean currents as well as the oxygen distribution in the ocean are changing. For example, the oxygen content in the ocean has decreased globally by about 2% in the last 60 years, in particular in the tropical oceans. However, in these regions complex and strongly fluctuating ocean currents also exist. At the equator, one of the strongest currents, the Equatorial Undercurrent (EUC), transports water masses eastwards across the Atlantic. For many years, scientists at GEOMAR have been investigating fluctuations of this current with fixed observation platforms, so-called moorings, in cooperation with the international PIRATA programme. Based on the data obtained from these moorings, they were able to prove that the EUC has strengthened by more than 20% between 2008-2018. The strengthening of this ocean current is also associated with increasing oxygen concentrations in the equatorial Atlantic and an increase in the oxygen-rich layer near the surface. This also means an extension of the habitat for tropical pelagic fish. The results of the study have now been published in the international journal Nature Geoscience.
“At first, this statement sounds encouraging, but it does not describe the entire complexity of the system”, says project leader and first author Prof. Dr. Peter Brandt from GEOMAR. “We found that the strengthening of the Equatorial Undercurrent is mainly caused by a strengthening of the trade winds in the western tropical North Atlantic”, Peter Brandt explains. The analysis of a 60-year data set has shown that the recent oxygen increase in the upper equatorial Atlantic is associated with a multidecadal variability characterised by low oxygen concentrations in the 1990s and early 2000s and high concentrations in the 1960s and 1970s. “In this respect, our results do not contradict the global trend, but show the need for long-term observations in order to be able to separate natural fluctuations of the climate system from trends such as oxygen depletion caused by climate warming”, says Brandt.
Read more at: Helmholtz Centre for Ocean Research Kiel (Geomar)
