In this concise report, we will look how different meteorological parameters changed during the dimming of the sun. Fortunately the cloud cover became thin enough during many moments to see the solar crescent. However the cloud cover remained so thick that looking at the solar crescent was possible without any protective glasses or other devices.
Atmospheric pressure increases a little due to the higher density of colder air.
Often solar eclipses go together with a more or less strong wind being produced by the pressure differences between the locally cooled down air and the more or less constant temperature of the air outside the shadow-zone. The poor sky condition prevented extreme variations in temperature and wind speed. The solar eclipse affected UVB and ozone values in a predictable manner.