基于卫星的降雨表征热带泥炭地水文响应:以文莱为例研究

IF 2.9 3区 地球科学 Q1 Environmental Science
Sebastian Apers, Alexander R. Cobb, Gabriëlle J. M. De Lannoy, Michel Bechtold
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引用次数: 0

摘要

泥炭的水力特性在调节热带泥炭地水文中起着至关重要的作用,因此是泥炭地特定水文模型的关键参数。泥炭的水力和排放参数可以通过分析原地水位和降水的时间序列以及地形数据来估计。然而,在植被密集和偏远的热带泥炭地,通常无法获得接近水位测量的现场降水数据。网格化卫星降水产品提供了另一种选择,但粗糙且高度不确定。在这里,我们提出了一种基于卫星降水的水位动态水文参数化方法,同时考虑了降水数据中的代表性误差。首先,我们采用Cobb和Harvey的水位上升和衰退分析(水资源研究,55 (11),9351-9377;2019),用于全球降水测量综合多卫星检索(IMERG)降水估计。应用于文莱的热带泥炭地,适应的上升和衰退分析减少了:(i)响应降雨的水位上升的平均误差和(ii)平均每日衰退的高估。此外,我们使用具有乘性误差的降水时间序列集合来量化我们的适应上升分析对降水误差的敏感性。其次,在NASA集水区陆面模型泥炭地特定模块中,利用调整后的总上升和下降曲线拟合土壤水力和流量功能参数。我们的分析可以使用IMERG数据为我们的案例研究检索准确的水文参数,并且可以转移到其他泥炭地和基于卫星的降水产品中。它还强调了云尺度强迫在热带泥炭地水文中的重要性,而这种强迫在现有的卫星降水产品中没有得到解决。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Characterising Tropical Peatland Hydrological Response With Satellite-Based Rainfall: A Case Study in Brunei

Characterising Tropical Peatland Hydrological Response With Satellite-Based Rainfall: A Case Study in Brunei

Peat hydraulic properties play a crucial role in regulating tropical peatland hydrology and are therefore critical parameters in peatland-specific hydrological models. Peat hydraulic and discharge parameters can be estimated by analysing time series of in situ water levels and precipitation, along with topographic data. However, in situ precipitation data are typically not available near water level measurements in densely vegetated and remote tropical peatlands. Gridded satellite precipitation products provide an alternative, but are coarse and highly uncertain. Here, we present a method for the hydrological parameterisation of water level dynamics using satellite-based precipitation, while accounting for representativeness errors in the precipitation data. First, we adapt the water level rise and recession analysis from Cobb and Harvey (Water Resources Research, 55 (11), 9351–9377; 2019) for use with Integrated Multi-satellitE Retrievals for Global Precipitation Measurement (IMERG) precipitation estimates. Applied to a tropical peatland in Brunei, the adapted rise and recession analysis reduces: (i) the average error in water level rise in response to rainfall and (ii) the average daily recession overestimation. In addition, we quantify the sensitivity of our adapted rise analysis to precipitation errors using an ensemble of precipitation time series with multiplicative errors. Second, the adapted master rise and recession curves are used to fit soil hydraulic and discharge function parameters within the peatland-specific module of the NASA Catchment Land Surface Model. Our analysis enables the retrieval of accurate hydrological parameters for our case study using IMERG data, and can be transferred to other peatlands and satellite-based precipitation products. It also highlights the importance in tropical peatland hydrology of cloud-scale forcing that is not resolved in existing satellite-based precipitation products.

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来源期刊
Hydrological Processes
Hydrological Processes 环境科学-水资源
CiteScore
6.00
自引率
12.50%
发文量
313
审稿时长
2-4 weeks
期刊介绍: Hydrological Processes is an international journal that publishes original scientific papers advancing understanding of the mechanisms underlying the movement and storage of water in the environment, and the interaction of water with geological, biogeochemical, atmospheric and ecological systems. Not all papers related to water resources are appropriate for submission to this journal; rather we seek papers that clearly articulate the role(s) of hydrological processes.
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