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全球变化对墨西哥中部两个热带高山湖泊的影响。

Impacts of global change on two tropical, high mountain lakes in Central Mexico.

作者信息

Ibarra-Morales Diana, Silva-Aguilera Raúl A, Oseguera Luis A, Merino-Ibarra Martín, Alcocer Javier

机构信息

Posgrado en Ciencias del Mar y Limnología, Universidad Nacional Autónoma de México, Av. Ciudad Universitaria 3000, Coyoacán, 04510 Ciudad de México, Mexico.

Grupo de Investigación en Limnología Tropical, Facultad de Estudios Superiores Iztacala, Universidad Nacional Autónoma de México, Av. de los Barrios No.1. Los Reyes Iztacala, 54090 Tlalnepantla, Estado de México, Mexico.

出版信息

Sci Total Environ. 2022 Dec 15;852:158521. doi: 10.1016/j.scitotenv.2022.158521. Epub 2022 Sep 5.

Abstract

High mountain lakes and their catchments are remote ecosystems in areas with low anthropogenic disturbance. High mountain lakes integrate changes in the atmosphere and catchment areas (e.g., acid rain, airborne pollutants, climate change). The present research analyses long-term datasets of meteorological and limnological variables representing two tropical high mountain lakes, El Sol and La Luna, in Central Mexico to identify the impacts of anthropogenic disturbance (i.e., sentinels of global/climate change). The 54-year meteorological analysis showed marked interannual variability with no statistically significant air temperature or rainfall trends. However, from 2000 to 2018, the air temperature increased by 0.5 °C. Accordingly, the lake water temperature increased (Lake El Sol: 0.8 °C, Lake La Luna: 0.6 °C). Although the rainfall displayed no change, the water level decreased in both lakes (1.5 m), most likely associated with increased evapotranspiration. Unexpectedly, the dissolved inorganic nitrogen (DIN) concentration in the lakes decreased. The initial acid pH rose to close neutrality in Lake La Luna and to alkaline values in Lake El Sol. The latter may be a consequence of the lowered SOx and NOx emissions from governmental regulations promulgated to control atmospheric pollution beginning in 2000 and probably resulting in less acidic deposition. An additional explanation for the lakes' deacidification is the increased deposition of alkaline ions derived from activities at the volcano slopes. Since the atmospheric supply is the primary nitrogen source to high mountain lakes, the DIN concentration decline could reflect the reduction in atmospheric HNO. Thus, Lakes El Sol and La Luna evidenced global change. Both lakes are inside the same crater and are subjected to similar influences; thus, they showed similar responses to global change (increasing lake water temperatures, declining water levels, higher pH value, and lower DIN concentrations). Nevertheless, their differences (e.g., catchment size, surface area, water volume, water depth, trophic status) influenced the magnitude of the impacts, with higher pH increases recorded in Lake El Sol and higher DIN concentrations in Lake La Luna.

摘要

高山湖泊及其集水区是人为干扰较少地区的偏远生态系统。高山湖泊综合了大气和集水区的变化(例如酸雨、空气传播污染物、气候变化)。本研究分析了代表墨西哥中部两个热带高山湖泊——埃尔索尔湖和拉卢纳湖的气象和湖沼学变量的长期数据集,以确定人为干扰的影响(即全球/气候变化的哨兵)。54年的气象分析显示出显著的年际变化,气温和降雨量没有统计学上的显著趋势。然而,从2000年到2018年,气温上升了0.5摄氏度。相应地,湖水温度也升高了(埃尔索尔湖:0.8摄氏度,拉卢纳湖:0.6摄氏度)。尽管降雨量没有变化,但两个湖泊的水位都下降了(1.5米),这很可能与蒸散量增加有关。出乎意料的是,湖泊中溶解无机氮(DIN)的浓度下降了。拉卢纳湖初始的酸性pH值上升至接近中性,而埃尔索尔湖则上升至碱性值。后者可能是由于2000年开始实施的旨在控制大气污染的政府法规降低了硫氧化物和氮氧化物的排放,可能导致酸性沉降减少。湖泊脱酸的另一个解释是火山斜坡活动产生的碱性离子沉积增加。由于大气供应是高山湖泊的主要氮源,DIN浓度下降可能反映了大气中HNO的减少。因此,埃尔索尔湖和拉卢纳湖证明了全球变化。两个湖泊位于同一个火山口内,受到相似的影响;因此,它们对全球变化表现出相似的反应(湖水温度升高、水位下降)。

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