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Benchmark products for land evapotranspiration: LandFlux-EVAL multi-data set synthesis

机译:陆地蒸散的基准产品:LandFlux-EVAL多数据集综合

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Land evapotranspiration (ET) estimates are available from several global data sets.Here, Monthly Global Land et Synthesis Products, Merged from These Individual Data Sets over the Time Periods 1989-1995 (7 Yr) and 1989-2005 (17 Yr), Are Presented. the Merged Synthesis Products over the Shorter Period Are Based on A Total of 40 Distinct Data Sets while Those over the Longer Period Are Based on A Total of 14 Data Sets. in the Individual Data Sets, et Is Derived from Satellite And/or in Situ Observations (Diagnostic Data Sets) or Calculated Via Land-surface Models (LSMs) Driven with Observations-based Forcing or Output from Atmospheric Reanalyses. Statistics for Four Merged Synthesis Products Are Provided, One Including All Data Sets and Three Including only Data Sets from One Category Each (Diagnostic, LSMs, and Reanalyses). the Multi-annual Variations of et in the Merged Synthesis Products Display Realistic Responses. They Are Also Consistent with Previous Findings of A Global Increase in et between 1989 and 1997 (0.13 Mm yr~(-2) in Our Merged Product) Followed by A Significant Decrease in This Trend (-0.18 Mm yr-2), although These Trends Are Relatively Small Compared to the Uncertainty of Absolute et Values. the Global Mean et from the Merged Synthesis Products (Based on All Data Sets) Is 493 Mm yr~(-1) (1.35 Mm d~(-1)) for Both the 1989-1995 and 1989-2005 Products, Which Is Relatively Low Compared to Previously Published Estimates. We Estimate Global Runoff (Precipitation Minus ET) to 263 Mm yr~ (-1) (34 406 km3 yr~(-1)) for A Total Land Area of 130 922 000 km2. Precipitation, Being An Important Driving Factor and Input to Most Simulated et Data Sets, Presents Uncertainties between Single Data Sets As Large As Those in the et Estimates. in Order to Reduce Uncertainties in Current et Products, Improving the Accuracy of the Input Variables, Especially Precipitation, As Well As the Parameterizations of ET, Are Crucial.
机译:可以从几个全球数据集获得土地蒸散量(ET)估算值。以下是1989-1995年(7年)和1989-2005年(17年)期间这些独立数据集合并的《全球月度土地及合成产品》,呈现。较短时期的合并合成产品基于总共40个不同的数据集,而较长时期的合并产品基于总共14个数据集。单个数据集中的“等”来自卫星和/或原位观测值(诊断数据集),或者通过基于观测值的强迫或大气再分析输出驱动的地表模型(LSM)计算得出。提供了四种合并的合成产品的统计信息,每种产品的统计信息来自一个类别(诊断,LSM和重新分析),其中一个包含所有数据集,三个仅包含数据集。合并后的合成产品中et的多年变化显示出现实的响应。它们也与以前的发现一致,即1989年至1997年期间全球et al增长(我们的合并产品中为0.13 Mm yr〜(-2)),随后这一趋势显着下降(-0.18 Mm yr-2),尽管这些与绝对值和不确定性相比,趋势相对较小。 1989-1995年和1989-2005年产品的合并平均值(基于所有数据集)得出的全球平均值为493 Mm yr〜(-1)(1.35 Mm d〜(-1))与先前发布的估算值相比较低。我们估算总径流(降水减去ET)为263 Mm yr〜(-1)(34 406 km3 yr〜(-1)),总土地面积为130922 000 km2。降水是大多数模拟的et数据集的重要驱动因素和输入,它表示与et估计中的数据集一样大的单个数据集之间的不确定性。为了减少当前产品的不确定性,提高输入变量(尤其是降水)以及ET的参数化的准确性至关重要。

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