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The exchange of water and energy between a tropical peat forest and the atmosphere: Seasonal trends and comparison against other tropical rainforests

机译:热带泥炭森林与大气之间的水和能量交换:季节性趋势以及与其他热带雨林的比较

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摘要

Tropical rainforests control the exchange of water and energy between the land surface and the atmosphere near the equator and thus play an important role in the global climate system. Measurements of latent (LE) and sensible heat exchange (H) have not been synthesized across global tropical rainforests to date, which can help place observations from individual tropical forests in a global context. We measured LE and H for four years in a tropical peat forest ecosystem in Sarawak, Malaysian Borneo using eddy covariance, and hypothesize that the study ecosystem will exhibit less seasonal variability in turbulent fluxes than other tropical ecosystems as soil water is not expected to be limiting in a tropical forested wetland. LE and H show little variability across seasons in the study ecosystem, with LE values on the order of 11 MJ m(-2) day and H on the order of 3 MJ m(-2) day(-1). Annual evapotranspiration (ET) did not differ among years and averaged 1579 +/- 47 mm year(-1). LE exceeded characteristic values from other tropical rainforest ecosystems in the FLUXNET2015 database with the exception of GF-Guy near coastal French Guyana, which averaged 8-11 MJ m(-2) day(-1). The Bowen ratio (Bo) in tropical rainforests in the FLUXNET2015 database either exhibited little seasonal trend, one seasonal peak, or two peaks. Volumetric water content (VWC) and VPD explained a trivial amount of the variability of LE and Bo in some of the tropical rainforests including the study ecosystem, but were strong controls in others, suggesting differences in stomatal regulation and/or the partitioning between evaporation and transpiration. Results demonstrate important differences in the seasonal patterns in water and energy exchange across different tropical rainforest ecosystems that need to be understood to quantify how ongoing changes in tropical rainforest extent will impact the global climate system. (C) 2019 Elsevier B.V. All rights reserved.
机译:热带雨林控制着陆地表面与赤道附近大气之间的水和能量交换,因此在全球气候系统中发挥着重要作用。迄今为止,尚未对全球热带雨林的潜热(LE)和显热交换(H)进行测量,这有助于在全球范围内对单个热带森林进行观测。我们使用涡度协方差对马来西亚婆罗洲沙捞越的热带泥炭森林生态系统中的LE和H进行了四年的测量,并假设与其他热带生态系统相比,研究生态系统的湍流通量季节变化性较小,因为预计土壤水不会受到限制在热带森林湿地。 LE和H在研究生态系统中随季节变化不大,LE值为11 MJ m(-2)天,H值为3 MJ m(-2)day(-1)。年蒸发蒸腾量(ET)年间无差异,平均年蒸发量为1579 +/- 47毫米(-1)。 LE超出FLUXNET2015数据库中其他热带雨林生态系统的特征值,但法属圭亚那沿海附近的GF-Guy除外,其平均8-11 MJ m(-2)天(-1)。 FLUXNET2015数据库中热带雨林的鲍文比(Bo)显示出很少的季节趋势,一个季节峰值或两个峰值。体积水含量(VWC)和VPD解释了包括研究生态系统在内的某些热带雨林中LE和Bo的微不足道的变化,但在其他热带雨林中却是强力控制,表明气孔调节和/或蒸发与水分分配之间存在差异。蒸腾作用。结果表明,不同热带雨林生态系统中水和能源交换的季节性模式存在重要差异,需要对其进行量化,以量化热带雨林范围内持续变化将如何影响全球气候系统。 (C)2019 Elsevier B.V.保留所有权利。

著录项

  • 来源
    《The Science of the Total Environment》 |2019年第15期|166-174|共9页
  • 作者单位

    Montana State Univ, Dept Land Resources & Environm Sci, Bozeman, MT 59717 USA|Sarawak Trop Peat Res Inst, Lot 6035,Kuching Kota Samarahan Expressway, Kota Samarahan 94300, Sarawak, Malaysia;

    Montana State Univ, Dept Land Resources & Environm Sci, Bozeman, MT 59717 USA;

    Natl Inst Environm Studies, Ctr Global Environm Res, Tsukuba, Ibaraki 3058506, Japan;

    Sarawak Trop Peat Res Inst, Lot 6035,Kuching Kota Samarahan Expressway, Kota Samarahan 94300, Sarawak, Malaysia;

    Sarawak Trop Peat Res Inst, Lot 6035,Kuching Kota Samarahan Expressway, Kota Samarahan 94300, Sarawak, Malaysia;

    Sarawak Trop Peat Res Inst, Lot 6035,Kuching Kota Samarahan Expressway, Kota Samarahan 94300, Sarawak, Malaysia;

    Civil Engn Res Inst Cold Reg, Sapporo, Hokkaido 0628602, Japan;

    Sarawak Trop Peat Res Inst, Lot 6035,Kuching Kota Samarahan Expressway, Kota Samarahan 94300, Sarawak, Malaysia;

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  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    Eddy covariance; FLUXNET; Latent heat flux; Sensible heat flux; Tropical peat forest; Tropical rainforest;

    机译:涡协方差;FLUXNET;潜热通量;感热通量;热带泥炭林;热带雨林;
  • 入库时间 2022-08-18 04:24:23

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