首页> 外文期刊>Hydrological Processes >Rainfall and fog interception at the lower and upper altitudinal limits of cloud forest in Veracruz, Mexico
【24h】

Rainfall and fog interception at the lower and upper altitudinal limits of cloud forest in Veracruz, Mexico

机译:墨西哥韦拉克鲁斯州云林海拔高度上限和下限的降雨和雾气拦截

获取原文
获取原文并翻译 | 示例
           

摘要

Comparisons of rainfall and fog interception among different types of tropical mon-tane cloud forest usually reveal large differences, but the variation in these processes within a given forest type has rarely been studied. In the present study, the altitudinal variation of rainfall (I-p) and fog (I-f) interception was investigated for a lower mon-tane cloud forest in central Veracruz, Mexico. For this, rainfall (P), net rainfall, fog presence (visibility), and meteorological variables were measured in the "Santuario" natural reserve (1,300 m asl) during two sampling periods that were representative of the dry and wet seasons, respectively. In addition, the canopy water storage capacity (C-m) was determined. The results were then compared with data published for the "Cortadura" reserve (2,170 m). There was no evidence of I-f in Santuario, whereas it was estimated at 8% of the dry-season P in Cortadura. In Santuario, relative I-p was 22% and 9% of P during the dry and wet seasons, respectively (compared with 20% and 18% of P, respectively, in Cortadura). Average rainfall event size and C-m were the main factors determining the relative I-p at both sites. C-m was much lower in Santuario (1.0 mm) than in Cortadura (3.9 and 2.8 mm in the wet and dry seasons, respectively). However, because during the dry season the average rainfall event size was much lower in Santuario, relative I-p was similar between sites. In contrast, during the wet season, the average event size was similar between sites, so that the difference in C-m caused an important altitudinal variation in relative I-p.
机译:通常,对不同类型的热带单峰云森林之间的降雨和雾气截留进行比较后,发现差异很大,但是很少研究给定森林类型中这些过程的变化。在本研究中,对墨西哥中部韦拉克鲁斯州较低的单峰云林调查了降雨(I-p)和雾(I-f)截留的高度变化。为此,在代表干燥季节和湿润季节的两个采样期中,在“ Santuario”自然保护区(1300 m asl)中测量了降雨(P),净降雨,雾的存在(能见度)和气象变量,分别。另外,确定冠层储水量(C-m)。然后将结果与为“ Cortadura”储量(2,170 m)发布的数据进行比较。 Santuario没有I-f的证据,而Cortadura的I-f估计为旱季P的8%。在Santuario,相对I-p在干季和湿季分别为P的22%和9%(相比之下,Cortadura中P的分别为20%和18%)。平均降雨事件的大小和C-m是决定两个地点相对I-p的主要因素。 Santuario的C-m(1.0 mm)远低于Cortadura(湿季和旱季分别为3.9和2.8 mm)。但是,由于在干旱季节,Santuario的平均降雨事件规模要小得多,因此两个站点之间的相对I-p相似。相反,在雨季,站点之间的平均事件大小相似,因此C-m的差异引起相对I-p的重要海拔变化。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号