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About climate change and how it influences the outflow of „green” versus „blue” water from the mountains

It’s a paradox: while streams dry up in hot summers, the vegetation at medium and high elevations is lush and green. Photo: iStock/gkuna

Researchers at ETH Zurich explain the phenomenon that in dry periods vegetation at high altitude grows better than normal / Far-reaching consequences

Until now, it was assumed that most plants suffer from water stress during droughts: they close their stomata to retain water, stop growing and, in the worst case, wither. As a result, there is a decrease in evaporation and transpiration of water from vegetation, soil and water surfaces – a process that experts call evapotranspiration. „But despite dry and warm conditions, droughts are not occurring at higher altitudes in, say, forested mountain areas,” says Simone Fatichi, senior assistant at the ETH Zurich Institute of Environmental Engineering.

Analyses of observations and computer model simulations from the heat wave of summer 2003 (and recent hot and dry summers) indicate that, during droughts, mountain forests and grasslands at higher elevations release even more water into the air than in usual periods of growth with average temperatures and sufficient precipitation.

This is because warmth and abundant sunshine promote vegetation growth. But at the same time, the vegetation has a higher metabolism, and so it essentially sucks every last drop of water from the ground in order to grow. For that reason, evapotranspiration was much greater than expected at higher altitudes during the droughts studied.

Fatichi and his colleagues have now investigated this phenomenon across large areas in the European Alps for the first time, with the help of a computer model. This enabled them to quantify the share of „green” water, i.e. water that reaches the air through evapotranspiration, in proportion to that of „blue” water, the water that runs off into streams, rivers and lakes.

On the basis of their simulation, Fatichi and his doctoral student Theodoros Mastrotheodoros calculated that in forested mountain areas 1,300 – 3,000 m above sea level, evapotranspiration rates were above average in large parts of the Alps during the heat wave of 2003.

That summer, Alpine water fluxes were on average only half their usual volume and, according to the ETH researchers’ calculations, one third of this runoff deficit was attributable to evapotranspiration. Fatichi emphasizes that „it is therefore the vegetation at this altitude that was instrumental in draining the half-dry rivers and streams.”

In an average summer (left), less water evaporates through vegetation; in a hot summer accompanied by dry conditions, the opposite is true, which amplifies the lack of water in streams. Graphic: Michael Stünzi / ETH Zürich

As part of their investigation, the researchers also simulated a temperature rise of 3 degrees in the Alpine region – a scenario that could become reality by the end of this century and that could further increase annual evaporation rates by as much as 6 percent. In terms of precipitation, the amount of evaporated water would be comparable to an annual decline in the Alps of 45 liters per square meter on average – which corresponds to 3–4 percent of annual precipitation. This remarks that at the annual scale – differently from warm summers – precipitation and its changes are by far the most important factors that determine runoff volumes.

As a result, discharge volumes in rivers and streams will come under even greater pressure in future. „As summers become warmer and drier, we’ll see a shift towards more green and less blue water,” Fatichi says. In the long term, this will endanger the supply of water to the lower-lying regions in and around the Alps, he explains.

Several factors play into this scenario: global warming is expected to result in a general reduction in precipitation, glaciers are set to dwindle and, in dry and warm summers, evapotranspiration will intensify the problem of lower runoff volumes. Such circumstances could cast some doubt over the Alps’ role as the „water towers of Europe”. Four of Europe’s major rivers, the Rhine, Rhône, Inn and Po, originate in the Alps. Together, they supply around 170 million people with water and play a crucial role in power generation and agriculture.

A large part of Europe therefore depends on the blue water from the Alps, leading Fatichi to ask the question, „can we really afford to allow the volumes of this water to decline?“

Mastrotheodoros T, et al. More green and less blue water in the Alps during warmer summers. Nature Climate Change, published online 27th 2019, doi: 10.1038/s41558-019-0676-5

Source: Eidgenössische Technische Hochschule (ETH) Zürich

(04.02.2020, USA: 02.04.2020)