森林河流流域水文循环模拟及森林采伐的水文后果

L. Kuchment, A. Gelfan, V. Demidov
{"title":"森林河流流域水文循环模拟及森林采伐的水文后果","authors":"L. Kuchment, A. Gelfan, V. Demidov","doi":"10.2174/1874378101105010009","DOIUrl":null,"url":null,"abstract":"Physically based model of the hydrological cycle of a forest basin was developed. The model includes descrip- tion of processes of liquid water and snow interception by forest canopy, snow accumulation and melt, vertical soil mois- ture transfer and evapotranspiration, overland, subsurface and channel flow. The case-study has been carried out on the basis of experimental observations on the Valday water balance station, situated in the north-western part of Russia. The model has been calibrated and validated using 5-year hydrometeorological observations at the completely forested Tayoz- hny Creek experimental basin. Then the 17-years hydrometeorological observations were used to estimate the possible change of hydrological cycle of this basin after forest cutting. The numerical experiments have shown that the averaged snow water equivalent before snowmelt for the Tayozhny Creek basin can increase in case of forest cutting by 15%. The snow sublimation losses can decrease almost twice .The snowmelt rates after forest cutting turned out to be about 30% larger and the duration of snowmelt, on average, on 10 days longer. The simulated annual runoff from the Tayozhny Creek basin (mainly of snowmelt origin) averaged for 17 years appeared to be only about 10% higher than in case of for- est cutting. However, its seasonal distribution and water balance components changed essentially. The spring flood peak discharge from the forested basin appeared to be, on average, 50% lower, the spring floods started 5-7 days later and the flood recession turned out to be much longer. About 80% of the total runoff from the Tayozhny Creek basin is now sub- surface flow, while in case of deforestation overland flow may become dominant. The numerical experiments were carried out to estimate the sensitivity of the hydrological cycle to changes of leaf area index as a forest age characteristic. The es- timates obtained by simulation are quite consistent with the estimates obtained on the basis of experimental research.","PeriodicalId":247243,"journal":{"name":"The Open Hydrology Journal","volume":"120 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2011-03-11","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"4","resultStr":"{\"title\":\"Modeling of the Hydrological Cycle of a Forest River Basin and Hydrological Consequences of Forest Cutting\",\"authors\":\"L. Kuchment, A. Gelfan, V. Demidov\",\"doi\":\"10.2174/1874378101105010009\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"Physically based model of the hydrological cycle of a forest basin was developed. The model includes descrip- tion of processes of liquid water and snow interception by forest canopy, snow accumulation and melt, vertical soil mois- ture transfer and evapotranspiration, overland, subsurface and channel flow. The case-study has been carried out on the basis of experimental observations on the Valday water balance station, situated in the north-western part of Russia. The model has been calibrated and validated using 5-year hydrometeorological observations at the completely forested Tayoz- hny Creek experimental basin. Then the 17-years hydrometeorological observations were used to estimate the possible change of hydrological cycle of this basin after forest cutting. The numerical experiments have shown that the averaged snow water equivalent before snowmelt for the Tayozhny Creek basin can increase in case of forest cutting by 15%. The snow sublimation losses can decrease almost twice .The snowmelt rates after forest cutting turned out to be about 30% larger and the duration of snowmelt, on average, on 10 days longer. The simulated annual runoff from the Tayozhny Creek basin (mainly of snowmelt origin) averaged for 17 years appeared to be only about 10% higher than in case of for- est cutting. However, its seasonal distribution and water balance components changed essentially. The spring flood peak discharge from the forested basin appeared to be, on average, 50% lower, the spring floods started 5-7 days later and the flood recession turned out to be much longer. About 80% of the total runoff from the Tayozhny Creek basin is now sub- surface flow, while in case of deforestation overland flow may become dominant. The numerical experiments were carried out to estimate the sensitivity of the hydrological cycle to changes of leaf area index as a forest age characteristic. The es- timates obtained by simulation are quite consistent with the estimates obtained on the basis of experimental research.\",\"PeriodicalId\":247243,\"journal\":{\"name\":\"The Open Hydrology Journal\",\"volume\":\"120 1\",\"pages\":\"0\"},\"PeriodicalIF\":0.0000,\"publicationDate\":\"2011-03-11\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"4\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"The Open Hydrology Journal\",\"FirstCategoryId\":\"1085\",\"ListUrlMain\":\"https://doi.org/10.2174/1874378101105010009\",\"RegionNum\":0,\"RegionCategory\":null,\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"\",\"JCRName\":\"\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"The Open Hydrology Journal","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.2174/1874378101105010009","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 4

摘要

建立了森林流域水文循环的物理模型。该模型包括森林冠层截流液态水和积雪过程、积雪积累和融化过程、垂直土壤水分转移和蒸散过程、地表、地下和河道流动过程的描述。案例研究是在位于俄罗斯西北部的瓦尔代水平衡站的实验观测基础上进行的。该模型已在完全森林覆盖的塔伊兹河实验流域进行了5年水文气象观测,并进行了标定和验证。利用17年水文气象观测资料,估算了森林采伐后该流域水循环可能发生的变化。数值试验表明,在森林砍伐15%的情况下,塔奥兹尼河流域融雪前的平均雪水当量可以增加。森林采伐后的融雪率提高了30%左右,融雪持续时间平均延长了10天。模拟的Tayozhny河流域(主要是融雪源)17年的年平均径流量似乎只比est砍伐情况高10%左右。但其季节分布和水分平衡成分发生了本质变化。森林流域的春季洪峰流量平均降低50%,春季洪水开始时间晚5 ~ 7天,洪水衰退时间更长。塔奥兹尼河流域大约80%的径流是地下流,而在森林砍伐的情况下,地面流可能占主导地位。通过数值试验研究了水循环对叶面积指数变化的敏感性。通过仿真得到的es-估计与实验研究得到的估计基本一致。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
Modeling of the Hydrological Cycle of a Forest River Basin and Hydrological Consequences of Forest Cutting
Physically based model of the hydrological cycle of a forest basin was developed. The model includes descrip- tion of processes of liquid water and snow interception by forest canopy, snow accumulation and melt, vertical soil mois- ture transfer and evapotranspiration, overland, subsurface and channel flow. The case-study has been carried out on the basis of experimental observations on the Valday water balance station, situated in the north-western part of Russia. The model has been calibrated and validated using 5-year hydrometeorological observations at the completely forested Tayoz- hny Creek experimental basin. Then the 17-years hydrometeorological observations were used to estimate the possible change of hydrological cycle of this basin after forest cutting. The numerical experiments have shown that the averaged snow water equivalent before snowmelt for the Tayozhny Creek basin can increase in case of forest cutting by 15%. The snow sublimation losses can decrease almost twice .The snowmelt rates after forest cutting turned out to be about 30% larger and the duration of snowmelt, on average, on 10 days longer. The simulated annual runoff from the Tayozhny Creek basin (mainly of snowmelt origin) averaged for 17 years appeared to be only about 10% higher than in case of for- est cutting. However, its seasonal distribution and water balance components changed essentially. The spring flood peak discharge from the forested basin appeared to be, on average, 50% lower, the spring floods started 5-7 days later and the flood recession turned out to be much longer. About 80% of the total runoff from the Tayozhny Creek basin is now sub- surface flow, while in case of deforestation overland flow may become dominant. The numerical experiments were carried out to estimate the sensitivity of the hydrological cycle to changes of leaf area index as a forest age characteristic. The es- timates obtained by simulation are quite consistent with the estimates obtained on the basis of experimental research.
求助全文
通过发布文献求助,成功后即可免费获取论文全文。 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
Editorial: Hydrology and the Environment Mitigation and Adaptation Responses to Sea Level Rise Mohid Land - Porous Media, a Tool for Modeling Soil Hydrology at PlotScale and Watershed Scale Wealth of the Oceans Innovations Related to Hydrology in Response to Climate Change - A Review
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1