Relationship between pollution and rainfall: how much water falls in the mountains and in the lowland can depend on the atmospheric aerosols.
Living in a period of strong impact of human activity on the environment and climatic variations, it is reasonable to ask whether the distribution of rainfall between lowland and mountain is stable or not. To this end, rainfall data has been analyzed in the Alpine region at different altitudes.
Did you ever get to top of
the mountain? Beautiful landscapes, the tingling air, the emotion of
being part of nature, the silence, the opportunity of looking at the
world from another point of view, impressive and fascinating clouds,
storms.. Passion can often be the reason behind decision to undertake
a path, and perhaps because of it I started to study physical
environmental processes during my University career.
Fig.1: Orographic clouds on the Sella pass, third of seven Dolomites mountain passes in Italy.
When I was studying for my
bachelor degree, I was very lucky because I got to know Claudia
Pasquero who encouraged me to follow this complex and fascinating
path. We started together to study precipitation in areas with
complex orography during my master thesis, maybe because we were
driven by environmental passion,
but basically because mountains are a fundamental
reservoir of fresh water for humanity and since
of precipitation are expected in the
changing climate, it becomes particularly important to understand how
orographic precipitation responds to global warming and to
anthropogenic forcing; this topic, unfortunately, have not been yet
investigated in depth. Our
goal was basically to determine whether the orographic enhancement of
precipitation was stable over the years or whether it changed over
time, but we had a doubt: which kind of
observational dataset could we use? Unfortunately in this field
large amount of data is in historical archives, and also in the 1990s
many mechanical rain gauges were dismissed and replaced with
automatic instruments without a good calibration, and thus the time
series couldn’t and cannot be merged to generate longer time
series. But at that time I was lucky once again: during my master I
met a group of the University of Milano who after 10 years of
activities released two beautiful precipitation datasets: one
providing homogenized monthly precipitation (1961-1990) in the
Italian Alpine region and the second one delivering a longer digitized
historical monthly precipitation dataset in a Northern Italian
region. So, a light bulb just went off in my head: "We can analyze
Fig. 2: Stations of the high density database used in the study and relative annual mean precipitation.
We started to do statistical analysis of the temporal series and after more than one year and a half of work, something was discovered: from the middle of the last century to the 1980s, the rains in the lowland stations decreased while on the heights there was no reduction; in the following period and until now lowland rainfall increased with respect to mountain rainfall. This result surprised us: while a decrease in rainfall is considered a possible effect of global warming in the area, the difference in behavior between rainfall at different altitudes is a new result! We noted also that the greatest difference between rainfall at high altitude and lowlands observed in the 1980s could be due to pollutants. In fact, pollution related to human activities had a similar pattern, with the peak of pollution reached in the mid-1980s and the subsequent decrease associated with the introduction of regulatory limits. The mechanisms underlying the link between pollution and rain can be different, in fact the pollution plays a role in the formation of clouds, and furthermore can modify the atmospheric dynamic.
The orographic enhancement of precipitation dependence on anthropogenic forcing is an important research line, but such as on mountain, if we are passionate, if we are determined and if we are curious, we can always do a step more.