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Hydrology of inland tropical lowlands: the Kapuas and Mahakam wetlands

机译:内陆热带低地水文:Kapuas和Mahakam湿地

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Wetlands are important reservoirs of water, carbon and biodiversity. They are typical landscapes of lowland regions that have high potential for water retention. However, the hydrology of these wetlands in tropical regions is often studied in isolation from the processes taking place at the catchment scale. Our main objective is to study the hydrological dynamics of one of the largest tropical rainforest regions on an island using a combination of satellite remote sensing and novel observations from dedicated field campaigns. This contribution offers a comprehensive analysis of the hydrological dynamics of two neighbouring poorly gauged tropical basins; the Kapuas basin (98 700 km(2)) in West Kalimantan and the Mahakam basin (77 100 km(2)) in East Kalimantan, Indonesia. Both basins are characterised by vast areas of inland lowlands. Hereby, we put specific emphasis on key hydrological variables and indicators such as discharge and flood extent. The hydroclimatological data described herein were obtained during fieldwork campaigns carried out in the Kapuas over the period 2013-2015 and in the Mahakam over the period 2008-2010. Additionally, we used the Tropical Rainfall Measuring Mission (TRMM) rainfall estimates over the period 1998-2015 to analyse the distribution of rainfall and the influence of El-Nino -Southern Oscillation. Flood occurrence maps were obtained from the analysis of the Phase Array type L-band Synthetic Aperture Radar (PALSAR) images from 2007 to 2010. Drought events were derived from time series of simulated groundwater recharge using time series of TRMM rainfall estimates, potential evapotranspiration estimates and the threshold level approach. The Kapuas and the Mahakam lake regions are vast reservoirs of water of about 1000 and 1500 km(2) that can store as much as 3 and 6.5 billion m(3) of water, respectively. These storage capacity values can be doubled considering the area of flooding under vegetation cover. Discharge time series show that ba
机译:湿地是水、碳和生物多样性的重要水库。它们是低地地区的典型景观,具有很高的蓄水潜力。然而,热带地区这些湿地的水文研究往往与流域规模上发生的过程相隔离。我们的主要目标是利用卫星遥感和专门实地活动的新观测相结合,研究一个岛屿上最大的热带雨林地区之一的水文动力学。这篇文章对两个相邻的测量较差的热带盆地的水文动力学进行了全面分析;西加里曼丹的卡普亚斯盆地(98700km(2))和东加里曼丹的马哈坎盆地(77100km(2))。这两个盆地都有大片内陆低地。因此,我们特别强调关键水文变量和指标,如流量和洪水范围。本文所述的水文气候学数据是在2013-2015年期间在卡普亚斯和2008-2010年期间在马哈卡姆进行的实地调查中获得的。此外,我们还使用了1998-2015年期间的热带降雨测量任务(TRMM)降雨估算,分析了降雨分布和厄尔尼诺-南方涛动的影响。洪水发生图是通过分析2007年至2010年的相控阵L波段合成孔径雷达(PALSAR)图像获得的。利用TRMM降雨估计时间序列、潜在蒸散量估计时间序列和阈值水平法,从模拟地下水补给时间序列中得出干旱事件。卡普亚斯和马哈卡姆湖地区是大约1000公里(2公里)和1500公里(2公里)的大型水库,可分别储存多达30亿和65亿立方米的水。考虑到植被覆盖下的洪水面积,这些存储容量值可以加倍。出院时间序列显示ba

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