Trends and shifts in streamflow in Hawai'i, 1913-2008

被引:49
作者
Bassiouni, Maoya [1 ,2 ]
Oki, Delwyn S. [1 ]
机构
[1] US Geol Survey, Pacific Isl Water Sci Ctr, Honolulu, HI 96813 USA
[2] Ecole Polytech Fed Lausanne, Sch Architecture Civil & Environm Engn, Environm Sci & Engn Sect, CH-1015 Lausanne, Switzerland
关键词
streamflow; groundwater; base flow; trends; climate; Hawai"i; RAINFALL; WATER; PRECIPITATION; PACIFIC; FORESTS; WAVES; CYCLE;
D O I
10.1002/hyp.9298
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
This study addresses a need to document changes in streamflow and base flow (groundwater discharge to streams) in Hawaii during the past century. Statistically significant long-term (19132008) downward trends were detected (using the nonparametric MannKendall test) in low-streamflow and base-flow records. These long-term downward trends are likely related to a statistically significant downward shift around 1943 detected (using the nonparametric Pettitt test) in index records of streamflow and base flow. The downward shift corresponds to a decrease of 22% in median streamflow and a decrease of 23% in median base flow between the periods 19131943 and 19432008. The shift coincides with other local and regional factors, including a change from a positive to a negative phase in the Pacific Decadal Oscillation, shifts in the direction of the trade winds over Hawaii, and a reforestation programme. The detected shift and long-term trends reflect region-wide changes in climatic and land-cover factors. A weak pattern of downward trends in base flows during the period 19432008 may indicate a continued decrease in base flows after the 1943 shift. Downward trends were detected more commonly in base-flow records than in high-streamflow, peak-flow, and rainfall records. The decrease in base flow is likely related to a decrease in groundwater storage and recharge and therefore is a valuable indicator of decreasing water availability and watershed vulnerability to hydrologic changes. Whether the downward trends will continue is largely uncertain given the uncertainty in climate-change projections and watershed responses to changes. Copyright (c) 2012 John Wiley & Sons, Ltd.
引用
收藏
页码:1484 / 1500
页数:17
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