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During the time spanned by our data, the surface waters of the lake (0\u20135 m) warmed at rates of 0.2\u20130.9 \u00b0C per decade, depending on season. The temperature of the deep waters (50-m bottom) displayed a rising trend in a meromictic basin of the lake and a sawtooth pattern in the other basin, which is holomictic. Long-term variation in surfacewater temperature correlated to global warming and multidecadal variation in two climatic oscillations, the Atlantic Multidecadal Oscillation (AMO) and the East Atlantic Pattern (EA).However, we did not detect an influence of the EA on the lake's temperature (as separate from the effect of global warming). Moreover, the effect of the AMO, estimated to a maximum of +1 \u00b0C, was not sufficient to explain the observed temperature increase (+2\u20133 \u00b0C in summer). Based on regional climate projections, we predicted that the lake will continue to warm at least until the end of the 21st century. Our results strongly suggest that the warming of Lake Lugano is tied to globalclimate change. To sustain current ecosystem conditions in Lake Lugano, we suggest that manage- ment plans that curtail eutrophication and (or) mitigation of global warming be pursued.", "description": "9 p.", "publisher": { "@type": "Organization", "name": "Elsevier" }, "author": [ { "@type": "Person", "name": "Roberts, James jroberts@usgs.gov", "givenName": "James", "familyName": "Roberts", "email": "jroberts@usgs.gov", "identifier": { "@type": "PropertyValue", "propertyID": "ORCID", "value": "0000-0002-4193-610X", "url": "https://orcid.org/0000-0002-4193-610X" }, "affiliation": [ { "@type": "Organization", "name": "Colorado Water Science Center", "url": "https://www.usgs.gov/centers/colorado-water-science-center" }, { "@type": "Organization", "name": "Fort Collins Science Center", "url": "https://www.usgs.gov/centers/fort-collins-science-center" } ] }, { "@type": "Person", "name": "Lepori, Fabio", "givenName": "Fabio", "familyName": "Lepori", "affiliation": [ { "@type": "Organization", "name": 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