Multi-decadal trends of low clouds at the Tropical Montane Cloud Forests

J. Antonio Guzmán Q., Hendrik F. Hamann, G. Arturo Sanchez-Azofeifa
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Abstract

Clouds are critical to the biodiversity and function of Tropical Montane Cloud Forests (TMCF). These ecosystems provide vital services to humanity and are considered hotspots of endemism, given that the number of species is restricted to their microclimates. Cloudiness (e.g., the fraction of low-clouds) 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) 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. Thus, we hypothesize that recent traces of global warming over the last few decades have led to decreases in low-cloud cover on TMCFs. The previous study was also evaluated globally and among biogeographic realms to identify regional trends. We computed trends by aggregating hourly observations from ERA5 reanalysis and CHIRPS into annual averages and then used linear regressions to calculate slopes (i.e., rate of change) (Δ, year). Our results suggest that CF trends at the TMCFs range between -64.7 ×10 and 51.4 ×10 CF year, 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 ×10CF year; tropical landmasses -2.3 ×10 CF year). Despite this, CF trends tend to 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 a fingerprint of global change on TMCFs, highlighting a current threat to species and essential ecosystem services that these ecosystems provide.
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热带山地云雾林低云的多年代际变化趋势
云对热带山地云雾林(TMCF)的生物多样性和功能至关重要。这些生态系统为人类提供了至关重要的服务,由于物种数量受其小气候的限制,它们被认为是特有的热点地区。由于全球变暖,预计这些生态系统中的云量(如低云的比例)将减少,但近期的时间趋势仍不清楚。在这里,我们评估了1997年至2020年全球521个具有tmfc的站点的低云分数(CF)和其他基本气候变量(ECV)(如地表温度、压力、土壤湿度和降水)的趋势。因此,我们假设最近几十年全球变暖的痕迹导致了tmcf低云覆盖的减少。之前的研究还在全球和生物地理领域之间进行了评估,以确定区域趋势。我们通过将ERA5再分析和CHIRPS的每小时观测数据汇总为年平均值来计算趋势,然后使用线性回归来计算斜率(即变化率)(Δ, year)。我们的研究结果表明,在tmcf的CF趋势范围在-64.7 ×10和51.4 ×10CF年之间,表明70%的评估站点经历了CF的减少。当密度分布的峰值比较时,这些生态系统中低云的下降比热带大陆严重253% (tmcf: -7.8 ×10CF年;热带大陆-2.3 ×10 CF年)。尽管如此,在不同的生物地理领域,气候变化趋势是不同的,因为那些来自新热带和印度洋地区的tmcf下降最为明显。CF的减少还与地表温度和压力的增加以及土壤水分的减少有关,这表明TMCF的气候正在向更温暖的环境变化。这些气候变化可能代表了全球变化对tmcf的影响,突出了这些生态系统提供的物种和基本生态系统服务当前面临的威胁。
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