Abstract. An oxygen decrease of the intermediate-depth low-oxygen
zones (300 to 700 m) is seen in time series for selected tropical areas for
the period 1960 to 2008 in the eastern tropical Atlantic, the equatorial
Pacific and the eastern tropical Indian Ocean. These nearly 5-decade
time series were extended to 68 years by including rare historic data
starting in 1950 and more recent data. For the extended time series between
1950 and 2018, the deoxygenation trend for the layer 300 to 700 m is similar
to the deoxygenation trend seen in the shorter time series. Additionally,
temperature, salinity, and nutrient time series in the upper-ocean layer (50
to 300 m) of these areas were investigated since this layer provides
critical pelagic habitat for biological communities. Due to the low amount
of data available, the results are often not statistically significant within
the 95 % confidence interval but nevertheless indicate trends worth
discussing. Generally, oxygen is decreasing in the 50 to 300 m layer, except
for an area in the eastern tropical South Atlantic. Nutrients also showed
long-term trends in the 50 to 300 m layer in all ocean basins and indicate
overlying variability related to climate modes. Nitrate increased in all
areas. Phosphate also increased in the Atlantic Ocean and Indian Ocean areas,
while it decreased in the two areas of the equatorial Pacific Ocean.
Silicate decreased in the Atlantic and Pacific areas but increased in the
eastern Indian Ocean. Hence, oxygen and nutrients show trends in the tropical
oceans, though nutrients trends are more variable between ocean areas than
the oxygen trends; therefore, we conclude that those trends are more
dependent on local drivers in addition to a global trend. Different positive
and negative trends in temperature, salinity, oxygen and nutrients indicate
that oxygen and nutrient trends cannot be completely explained by local
warming.