Abstract. Multiple global change drivers affect plant productivity of grasslands and
thus ecosystem services like forage production and the soil carbon sink.
Subalpine grasslands seem particularly affected and may serve as a proxy for
the cold, continental grasslands of the Northern Hemisphere. Here, we
conducted a 4-year field experiment (AlpGrass) with 216 turf monoliths,
subjected to three global change drivers: warming, moisture, and
N deposition. Monoliths from six different subalpine pastures were
transplanted to a common location with six climate scenario sites (CSs). CSs
were located along an altitudinal gradient from 2360 to 1680 m a.s.l.,
representing an April–October mean temperature change of −1.4 to +3.0 ∘C, compared to CSreference with no temperature
change and with climate conditions comparable to the sites of origin. To
uncouple temperature effects along the altitudinal gradient from soil
moisture and soil fertility effects, an irrigation treatment (+12 %–21 %
of ambient precipitation) and an N-deposition treatment (+3 kg and +15 kg N ha−1 a−1) were applied in a factorial design, the latter
simulating a fertilizing air pollution effect. Moderate warming led to increased productivity. Across the 4-year
experimental period, the mean annual yield peaked at intermediate CSs
(+43 % at +0.7 ∘C and +44 % at +1.8 ∘C),
coinciding with ca. 50 % of days with less than 40 % soil moisture
during the growing season. The yield increase was smaller at the lowest,
warmest CS (+3.0 ∘C) but was still 12 % larger than at
CSreference. These yield differences among CSs were well explained by
differences in soil moisture and received thermal energy. Irrigation had a
significant effect on yield (+16 %–19 %) in dry years, whereas
atmospheric N deposition did not result in a significant yield response. We
conclude that productivity of semi-natural, highly diverse subalpine
grassland will increase in the near future. Despite increasingly limiting
soil water content, plant growth will respond positively to up to
+1.8 ∘C warming during the growing period, corresponding to
+1.3 ∘C annual mean warming.