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[Display omitted] • Low-cloud cover in cloud forests is declining. • Low-cloud trends over 23 years in 521 cloud forests were evaluated. • Seventy percent of the cloud forests experienced a decrease in low-clouds. • Cloud forests experience steeper declines in low-clouds than in tropical landmasses. • Low-cloud trends indicate potential threats to species and ecosystem services. Clouds are critical to the biodiversity and function of Tropical Montane Cloud Forests (TMCF) as they control water regimes and sunlight that can be perceived by plants. These ecosystems provide a key role in ecosystem services to humanity and are considered hotspots of endemism, given that the number of species is restricted to their microclimates. The cloudiness in these ecosystems is projected to decline owing to global warming, but recent temporal trends remain unclear. Here, we evaluated trends in low-cloud fractions (CF) (e.g., the proportion of an area covered by low-cloud) and other Essential Climatic Variables (ECV) (e.g., surface temperature, pressure, soil moisture, and precipitation) for 521 sites worldwide with TMFCs from 1997 to 2020. We hypothesize that recent traces of global warming over the last few decades have led to decreases in CF on TMCFs. The previous was also assessed globally and among biogeographic realms to identify regional trends. We calculated trends by aggregating hourly observations from ERA5 reanalysis and CHIRPS into annual averages and then using linear regressions to calculate slopes (i.e., rate of change) (Δ, year−1). Our results suggest that CF trends at the TMCFs range between −64.7×10−4 and 51.4×10−4 CF year−1, revealing that 70 % of the assessed sites have experienced reductions in CF. Declines in low-clouds in these ecosystems are 253 % more severe than tropical landmasses when peak values of density distribution are compared (TMCFs: −7.8×10−4 CF year−1; tropical landmasses −2.3×10−4 CF year−1). Despite this, CF trends differ among biogeographic realms, as those TMCFs from the Neotropics and Indomalayan realms have the most pronounced declines. Decreases in CF were also associated with increases in surface temperature and pressure and decreases in soil moisture, revealing that the TMCF's climate is changing to warmer environments. These climatic shifts may represent imprints of global change on TMCFs, highlighting a current threat to species and essential ecosystem services that these ecosystems provide. [ABSTRACT FROM AUTHOR]