Recently there was an article in the newspaper El diario de Mallorca where they were talking about the water temperature around the Balearic Islands, as it seems they reached very high values for this time of the year. Let’s have a look at that.
The SOCIB maintains several mooring around the islands, the
one we will use is located in the Bahía de Palma and provides data since 2014.
The data can be downloaded in netCDF format, but it is not necessary to download everything
since there is a possibility to access the information using the OPEnDAP
protocol.
When I was working there I wrote some python code to read and plot this kind of time series, I kind of did it on a rush, so it’s not the cleanest code I’ve seen, and probably it is necessary to edit it a little bit…
By the way, all the plotting tools are available in this GitHub project:
It turns out that the adaptation of the script was not too bad:
More of less 10 minutes of work, the bad part being the monthly file list: the file URL doesn’t not only depends on the year and month, but also on the deployment number and the ID of the platform. Sometimes they have to replace the sensor and this is reflected in the metadata and the file name. Anyway, that kind of issues for the data user should be overcome by the deployment of new Data API.
So here we are, the comparison of temperature from June to September, between 2014 and 2018. Many things may strike in the time series:
We see that the present temperatures are at the same level as in 2017, but that doesn’t mean that the rest of the season will follow this tendency, as some events may provoke an abrupt decrease of temperature in a matter of a couple of days.
As a bonus we also have the evolution of the salinity for the same period. It is not easy to interpret what happens in the signal as there is no clear pattern in the variable evolution.
The most striking feature is maybe the higher salinity values in August measured in 2014 and 2018, between 38 and 38.2 PSU, while the salinity situated around 37.2-37.4 in 2017. The differences might have a physical origin for instance the presence of different water masses or a stronger imbalance between evaporation and precipitation. Or the origin may come from the instruments themselves, their calibration was maybe different.
Whatever the reason, it’s something that deserves a particular attention and comparison with other sources of information such as satellite images or numerical models.