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Analyzing cloud base at local and regional scales to understand tropical montane cloud forest vulnerability to climate change

机译:分析地方和区域尺度的云基础,以了解热带山地云林对气候变化的脆弱性

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摘要

The degree to which cloud immersion provides water in addition torainfall, suppresses transpiration, and sustains tropical montane cloudforests (TMCFs) during rainless periods is not well understood. Climate andland use changes represent a threat to these forests if cloud base altituderises as a result of regional warming or deforestation. To establish abaseline for quantifying future changes in cloud base, we installed aceilometer at 100 m altitude in the forest upwind of the TMCF that occupiesan altitude range from ∼ 600 m to the peaks at 1100 m in the LuquilloMountains of eastern Puerto Rico. Airport Automated Surface Observing System (ASOS)ceilometer data, radiosondedata, and Cloud-Aerosol Lidar and Infrared Pathfinder SatelliteObservation (CALIPSO) satellite data were obtained to investigate seasonal cloudbase dynamics, altitude of the trade-wind inversion (TWI), and typical cloudthickness for the surrounding Caribbean region. Cloud base is rarelyquantified near mountains, so these results represent a first look atseasonal and diurnal cloud base dynamics for the TMCF. FromMay 2013 to August 2016, cloud base was lowest during the midsummer dryseason, and cloud bases were lower than the mountaintops as often in thewinter dry season as in the wet seasons. The lowest cloud bases mostfrequently occurred at higher elevation than 600 m, from 740 to 964 m. TheLuquillo forest low cloud base altitudes were higher than six other sites inthe Caribbean by ∼ 200–600 m, highlighting the importance of siteselection to measure topographic influence on cloud height. Proximity to theoceanic cloud system where shallow cumulus clouds are seasonally invariant inaltitude and cover, along with local trade-wind orographic lifting and cloudformation, may explain the dry season low clouds. The results indicatethat climate change threats to low-elevation TMCFs are not limited to the dryseason; changes in synoptic-scale weather patterns that increase frequency ofdrought periods during the wet seasons (periods of higher cloud base) mayalso impact ecosystem health.
机译:人们对云的浸入程度以及降雨,抑制蒸腾作用以及在无雨期维持热带山地森林(TMCF)的程度的了解尚不清楚。如果由于区域变暖或森林砍伐导致云底海拔升高,气候和土地利用的变化将对这些森林构成威胁。为了建立量化未来云量变化的基线,我们在TMCF上游森林的100 m处安装了电度计,该海拔高度范围从600 m到波多黎各东部Luquillo山脉的1100 m的峰值。获得了机场自动表面观测系统(ASOS)的高度计数据,无线电探空仪数据,云气溶胶激光雷达和红外探路者卫星观测(CALIPSO)卫星数据,以调查季节性云层动态,逆风高度(TWI)以及典型的云层厚度周围的加勒比地区。山区附近云量很少被量化,因此这些结果代表了TMCF季节性和昼夜云量动态的初步观察。从2013年5月到2016年8月,盛夏旱季的云量最低,冬季和旱季的云量通常低于山顶。最低的云层基数通常发生在海拔高度超过600 m的地方,从740到964 m。 Luquillo森林低云的基本高度比加勒比地区的其他六个站点高200〜600μm,这突出表明了选址对测量地形对云层高度影响的重要性。靠近洋云系统(浅积云是季节性不变的高度和覆盖面),以及局部信风地形的抬升和云的形成,可以解释干旱季节的低云。结果表明,气候变化对低海拔TMCF的威胁不仅限于旱季。天气尺度天气模式的变化会增加雨季干旱时期的频率(云量较高的时期),也可能影响生态系统的健康。

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