Annual and daily changes of the Amazon river water level
Annual and daily changes of the Amazon river water level
批准号:
11680089
负责人:
HIDA Noboru
金额:
$2.37万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (C)
财政年份:
1999
资助国家:
日本
项目状态:
已结题
起止时间:
1999 至 2002
中文摘要
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英文摘要
1. Armugl water level changes of the Amazon:The annual water level cycle of the Rio Negro reflects the rainfall characteristics, I.e., the wet and dry seasons in the drainage basin. The water level at Manaus normally reaches its peak in late June, and bottoms in late October. According to IBGE (1977, 1991), the water level begins to rise in early January, taking eight months to gradually approach its maximum, and then in late June it returns again to its lowest level within a period of four months.How high dose the annual maxima and minima reach? The data based on data from the Adinmistracao do Port de Manaus illustrates the 89 - year moving averages for the annual maxima and minima between 1903 and 1991.The Porto's data reveals that both the annual maximum and minimum varies from year to year. However, the maximum average annual water level is 27.70 m, and the standard deviation (σ) is 1.13, while the minimum average annual water level is 17.81 m, and the σ is 1.88 . The lowerσ for th … More e animal maximum water level as compared to the annual minimum water level can be understood by looking at the variation in the Porto's data as well. The difference between the maximum and the minimum water levels shows an average of 9.89 m (σ:1.89), I.e., about 10 m. The maximum spread between the two extremes is 14.13m (1909), and the minimum spread is 6.10 m (1969).2. Daily water level changes of the Amazon:Daily water level changes at Breves and Caxiuana, Amazon estuary show as follows:(1) As expected, the tidal cycles induce the water levels to rise and fall twice-a-day. Since Breves and Caciuana are situated almost on the equator, there is no appearance of diurnal inequality.(2) During the spring tides, associated wilh the full and new phases of the moon, the curves for water level changes almost coincide. However, they appear in a different pattern during the neap tides.(3) The variations between the high and low levels during the spring tides are 0.89m in April and 1.26m in November at Breves, and 0.20m in April and 0.27m in November at Caxiuana.(4) An irregular movement of water levels occurred around 17:00-18:00, in April owing to shipping disturbance.(5) There is a considerable time lag in the tides between Breves and Caciuana. The flood and ebb currents calculated from the time lag reach about 15km per hour. Less
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Kageyama, Yoichi: "Comparison of JERS-1 and Landsat TM data for estimating for water areas in the Amazon"Journal of Geography (Tokyo Geogrp. Society). 108・5. 552-561 (1999)
Kageyama, Yoichi:“用于估算亚马逊水域的 JERS-1 和 Landsat TM 数据的比较”地理杂志(东京地理学会)108・5(1999)。
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通讯作者:
Hiraoka, Mario: "Manejo tradicional de recursos naturales en el estuario del Rio Amazonas : Raphia Taedirera"Desarrollo sostenible en la Amazonia : mito o realidad, IFFA, ECUADOR. 133-198 (2001)
平冈,马里奥:“Manejo tradicional de recursos naturales en el Rio Amazonas : Raphia Taedirera”Desarrollo sostenible en la Amazonia : mito o realidad,IFFA,厄瓜多尔。
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Hida, Noboru: "Annual water level change of the Rio Negro river, Brazil"Geog. Rev. Japan. 76(Forthcoming). (2003)
Hida, Noboru:“巴西里奥内格罗河的年度水位变化”Geog。
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Mario Hiraoka: "Manejo tradicional de recursos naturales en el estuario del Rio Amazonas : Raphia Taedirera"Desarrollo sostenible en la Amazonia : mito o readidad, IFFA, ECUADOR. In Book. 133-198 (2001)
Mario Hiraoka:“Manejo tradicional de recursos naturees en el Rio Amazonas : Raphia Taedirera”Desarrollo sostenible en la Amazonia : mito o readidad,IFFA,厄瓜多尔。
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通讯作者:
Hida,Noboru, et al.: "River water level changes of the Amazon estuary : at Breves, Caxiuana and Abaetetuba"Intal.Sympo.Hydrol.and Geochem.Processe s: Manaus99 (Brazil). ABSTRACTS. 87 (1999)
Hida、Noboru 等人:“亚马逊河口的河流水位变化:在 Breves、Caxiuana 和 Abaetetuba”Intal.Sympo.Hydrol.and Geochem.Processes:Manaus99(巴西)。
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共 31 条
Reducing snow-removal works by using groundwater and artificial enhancement of groundwater cycle: Creation of the simultaneous realization model
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批准号:23650578
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项目类别:Grant-in-Aid for Challenging Exploratory Research
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资助金额:$1.41万
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财政年份:2011
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Field research on development and practical use of the optimum system of artificial groundwater recharge in Southeast Asian countries
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「Artificial Kecharge of Groundwater and Change of Groundwater Level」: For Progress of Control System
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项目类别:Grant-in-Aid for Scientific Research (B)
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资助金额:$2.56万
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财政年份:1999
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负责人:HIDA Noboru
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依托单位:
Water Level Change and Human Activity in the Amazon
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批准号:07041082
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资助金额:$7.42万
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财政年份:1995
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负责人:HIDA Noboru
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Research on the monitoring of groundwater level movement in alluvial fan
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批准号:03680207
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A study of groundwater management (development utilization conservation) in the Rokugo Alluvial Fan, Akita Prefectre
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负责人:HIDA Noboru
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依托单位:
海外基金