PDF(3185 KB)
PDF(3185 KB)
PDF(3185 KB)
西南诸河水文情势演变特征——以保山市为例
Evolution Characteristics of Hydrological Regimes in Rivers of Southwest China: Taking Baoshan City as an Example
[Objective] This paper aims to reveal the hydrological evolution patterns of transboundary rivers on the western Yunnan Plateau (the Lancang River, Nu River, and Irrawaddy River) during 1956-2016, to quantify the spatial differentiation characteristics of changes in water resources in the three major river systems, and to establish a water quantity prediction method based on multi-scale periodic analysis. [Methods] Based on precipitation and runoff data of the three major river systems in Southwest China from 1956 to 2016, the Mann-Kendall trend test method was used to analyze the long-term variation trends of hydrological elements. The Morlet wavelet analysis method was applied to identify the multi-scale periodic characteristics of hydrological sequences, and the phase extrapolation method was employed to predict future water quantity variation trends. [Results] The water yield modulus of the study area reached 78.83×104 m3/km2; however, all three river systems exhibited significant decreasing trends. Among them, the attenuation rate of the Irrawaddy River (-0.175×108 m3/a) was significantly higher than that of the Lancang River (-0.024×108 m3/a). A dominant 24-year hydrological variation period was identified at the regional scale, and the year 2016 was located at the end of the low-frequency phase of this cycle. Combined with phase extrapolation, the results indicated that future water quantity may continue to remain relatively low. The Lancang River exhibited secondary periodic oscillations of 7-12 years, which differed from the single dominant periodic pattern observed in the Nu River and the Irrawaddy River, revealing the hydrological response heterogeneity of the Lancang River caused by its specific underlying surface conditions. Precipitation showed a significant correlation with water resources (R2>0.75); however, asynchronous characteristics were observed in the Lancang River due to its specific underlying surface conditions. [Conclusion] This study systematically quantifies the spatial differentiation characteristics of hydrological evolution in the Lancang River, Nu River, and Irrawaddy River systems, establishes a water quantity prediction method based on multi-scale periodic analysis, and further reveals the secondary periodic oscillation characteristics of the Lancang River and its differences from the Nu River and Irrawaddy River, providing new scientific evidence for transboundary river water resources management in Southwest China. The results indicate that water resources of transboundary rivers on the western Yunnan Plateau may show a persistently low trend in the future, highlighting the need to strengthen transboundary water resources coordination and to formulate adaptive water resources allocation strategies.
水文情势 / 降水量 / 水资源量 / Mann-Kendall趋势检验 / Morlet小波分析 / 西南诸河
hydrological regime / precipitation / total water resources / Mann-Kendall trend test / Morlet wavelet analysis / rivers of Southwest China
| [1] |
|
| [2] |
张建云, 刘九夫, 金君良, 等. 青藏高原水资源演变与趋势分析[J]. 中国科学院院刊, 2019, 34(11):1264-1273.
(
|
| [3] |
Observations have shown that the hydrological cycle of the western United States changed significantly over the last half of the 20th century. We present a regional, multivariable climate change detection and attribution study, using a high-resolution hydrologic model forced by global climate models, focusing on the changes that have already affected this primarily arid region with a large and growing population. The results show that up to 60% of the climate-related trends of river flow, winter air temperature, and snow pack between 1950 and 1999 are human-induced. These results are robust to perturbation of study variates and methods. They portend, in conjunction with previous work, a coming crisis in water supply for the western United States.
|
| [4] |
刘春蓁. 气候变化对陆地水循环影响研究的问题[J]. 地球科学进展, 2004, 19(1): 115-119.
简要地回顾了现存的由气候情景驱动水文模型研究气候变化对陆地水循环影响的方法。指出这种单向连接方法很难将气候变暖及人类活动引起的陆地水循环变化反馈给大气。这既影响对降雨的预测精度,又不能正确地描写陆地水循环的变化。近10年来气候学家对大气环流模型中陆面过程模型的改进以及水文气候学家对大尺度水文模型研究所取得的进展,展现了它们之间的互补性,以及未来用水文-气候耦合模型方法研究气候变化与人类活动对陆地水循环影响及水资源预测的可能性。
(
|
| [5] |
乔时雨, 李国芳, 李国文, 等. 变化环境下赣江流域水文情势演变及归因分析[J]. 人民长江, 2024, 55(5): 99-106.
(
|
| [6] |
孔锋, 王一飞, 方建, 等. 中国不同月份和持续时间降雨的变化趋势与波动特征的空间格局对比研究(1961—2015)[J]. 首都师范大学学报(自然科学版), 2017, 38(6): 85-95.
(
|
| [7] |
程诗悦, 秦伟, 郭乾坤, 等. 近50年我国极端降水时空变化特征综述[J]. 中国水土保持科学, 2019, 17(3):155-161.
(
|
| [8] |
黄平, 周士杰. 全球变暖下热带降水变化研究回顾与挑战[J]. 地球科学进展, 2018, 33(11): 1181-1192.
热带降水是全球能量水份循环的重要环节。热带降水在全球变暖下的变化是目前国际上广泛关注的气候变化问题之一。回顾了近30年来关于热带降水在观测中的变化以及基于气候模式预估未来变化方面的研究进展;总结了目前在热带区域降水变化机制方面的国际前沿研究进展及研究方法;最后讨论了目前气候模式预估未来区域降水变化所遇到的模式间差异大等影响预估可信度的问题,展望未来研究中面临的主要挑战。
(
|
| [9] |
|
| [10] |
|
| [11] |
|
| [12] |
|
| [13] |
钟苏娟, 毛熙彦, 黄贤金. 地缘安全视角下的中国国际河流水资源开发利用[J]. 世界地理研究, 2022, 31(3): 466-477.
全球地缘政治竞争回潮与资源环境危机推动国际河流水资源开发利用成为影响国家地缘安全的关键变量。通过对既有文献的梳理,发现国际河流水资源开发利用在“稀缺-冲突”范式下激化流域各国的矛盾,引发的水资源冲突联合域外势力进一步作用于国家地缘安全;在地缘安全视角下,中国国际河流的水资源开发利用经历了从“弱安全化”到“强安全化”再到“去安全化”的演进;水环境治理、水量分配及水开发利益协调是水资源开发利用中的核心议题,涉及的跨境水资源污染、水权分配以及水电开发争议等问题与国家地缘安全密切相关;东北、西北及西南三大国际河流密集区水资源开发利用方式地域分异明显,在差异化的地缘环境下带来多元的地缘安全威胁;最后基于“一带一路”及“人类命运共同体”等背景对中国未来外交提出建议。
(
|
| [14] |
张宁, 陈文华, 李国永. 1981—2021年怒江下游勐波罗河降水演变及IOD关联[J]. 水电能源科学, 2025, 43(3): 22-25, 64.
(
|
| [15] |
吴绍洪, 潘韬, 曹杰, 等. 西南纵向岭谷地形对季风的“通道—阻隔”作用[J]. 地理研究, 2012, 31(1):1-13.
地形格局对大气环流与区域气候具有重要影响。已有研究认为纵向岭谷区主要受到印度洋季风与太平洋季风的共同影响,二者在哀牢山山脉附近交汇,哀牢山山脉是一条重要的地理分界线。本文从大气环流、水汽输送、区域气候、河川径流以及植物稳定氧同位素等多个方面研究发现:纵向岭谷地区主要受印度洋季风的影响,太平洋季风的影响在8月份有一定的作用,但不够明显;在地形格局作用下,地表水汽、降水以及河川径流在纵向岭谷区表现出明显的纬向差异、经向延伸的特征;大流环流、水汽输送、区域气候以及河川径流等的空间差异,是特殊环境对水热再分配的结果,即"通道-阻隔"作用的效应;这些差异不是地理地带性的表现,而是非地带性作用的结果;这种"通道—阻隔"作用导致地表水热条件的再分配,是该区生态地理格局形成与演化的主驱动力之一。纵向岭谷地形对季风的"通道—阻隔"作用导致了一系列地理要素的空间分异和相关联的生态效应。
(
|
| [16] |
|
| [17] |
|
| [18] |
陈文华, 徐娟, 李双成. 怒江流域下游地区气象与水文干旱特征研究[J]. 北京大学学报(自然科学版), 2019, 55(4): 764-772.
(
|
| [19] |
Selecting appropriate global climate models (GCMs) is crucial for minimizing uncertainty in regional climate projections under future scenarios. Previous studies have predominantly assessed the modeling capability of GCMs for regional precipitation climatology and its long-term patterns based on annual and seasonal precipitation data. Building upon these, we primally evaluated the performance of five GCMs from phase 3b of the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP3b) in simulating precipitation concentration and its variations in the Southwest River Basin (SWRB) of China using the precipitation concentration index (PCI). The results indicate that: (1) The 5 GCMs generally capture the spatial distribution of annual average precipitation in the SWRB but significantly overestimate its magnitude, with a maximum regional average deviation of 207.80 mm. Furthermore, all models tend to overestimate the overall drying trend in the SWRB and show limited capability in simulating interdecadal variations of annual precipitation. (2) While the 5 GCMs reasonably simulate the spatial distribution of annual average PCI in the SWRB, they tend to overestimate its values, with a maximum regional average deviation of 1.54. Additionally, their simulation performance in capturing PCI trends and interdecadal variations is also limited. (3) The 5 GCMs tend to overestimate seasonal precipitation in the SWRB, with the best simulation performance for the distribution of autumn precipitation, followed by spring and summer, and the poorest for winter. Significant differences exist in the simulation performance of the models for seasonal precipitation proportions, which result in discrepancies in the models' representation of PCI. Moreover, the models' poor simulation performance of PCI trends is partly due to their inadequate modeling of trends in seasonal precipitation proportions. The findings will contribute to laying the foundation for meteorological hydrological research and water resource management in the SWRB.© 2024. The Author(s).
|
| [20] |
南林江, 杨明祥, 郝少魁. 1965—2014年重庆地区降水时空分布特征分析[J]. 人民长江, 2021, 52(增刊2):64-69.
(
|
| [21] |
|
| [22] |
邹玉婷, 李昌文, 常文娟, 等. 湄公河三角洲洪水特性及其演变规律分析[J]. 人民长江, 2024, 55(3):35-41.
(
|
| [23] |
王文圣, 丁晶, 李跃清. 水文小波分析[M]. 北京: 化学工业出版社, 2005.
(
|
| [24] |
陈文华, 张宁, 冯春红, 等. 1981—2020年高黎贡山南段极端降水特性及演变趋势[J]. 长江科学院院报, 2025, 42(6): 44-50, 59.
为揭示高黎贡山南段极端降水时空变化特征及其与强ENSO事件的关系,基于1981—2020年区域8个站点的日降水数据,采用创新趋势分析(ITA)、线性回归分析(LR)以及复合分析等方法,以海温异常指数(DMI、ONI)为支持,选取5个极端降水指数(EPI)进行分析。结果显示:除最大连续干旱日数(CDD)显著增加外,大部分极端降水指标呈减少趋势,预示该地区存在干旱加剧的总体趋势,其中,东坡、西坡湿日总降水量(PTOT)减少幅度分别为39.9、46.1 mm/(10 a);最大连续干旱日数(CDD)增加幅度分别为3.9、0.7 d/(10 a);区域极端降水与大洋尼诺指数ONI存在弱到中等程度的关联,该关系主要表现为负相关,即ONI为正位相时,雨季降水更倾向为偏少(偏干)状态;在大尺度驱动因素的季节关联上,西、东坡流域略有差异。对前期和同期季节尺度ONI的跟踪将有助于对本地区极端降水变化作出预估。
(
|
| [25] |
刘冠华, 杨士力, 王化儒. 信阳市水资源时空变化特征研究[J]. 水文, 2024, 44(3): 74-81.
(
|
| [26] |
|
| [27] |
|
| [28] |
|
| [29] |
Both seasonal and annual mean precipitation and evaporation influence patterns of water availability impacting society and ecosystems. Existing global climate studies rarely consider such patterns from non-parametric statistical standpoint. Here, we employ a non-parametric analysis framework to analyze seasonal hydroclimatic regimes by classifying global land regions into nine regimes using late 20th century precipitation means and seasonality. These regimes are used to assess implications for water availability due to concomitant changes in mean and seasonal precipitation and evaporation changes using CMIP5 model future climate projections. Out of 9 regimes, 4 show increased precipitation variation, while 5 show decreased evaporation variation coupled with increasing mean precipitation and evaporation. Increases in projected seasonal precipitation variation in already highly variable precipitation regimes gives rise to a pattern of "seasonally variable regimes becoming more variable". Regimes with low seasonality in precipitation, instead, experience increased wet season precipitation.
|
| [30] |
苗正伟, 刘璐. 气候变化和人类活动对滹沱河上游流域水文干旱演变的影响[J]. 北京师范大学学报(自然科学版), 2024, 60(6): 870-880.
(
|
| [31] |
张晓莹, 何毅, 翁学先, 等. 秦巴山区堵河流域径流变化归因分析[J]. 长江科学院院报, 2024, 41(2):44-51.
(
|
/
| 〈 |
|
〉 |