高寒内陆河流域湿地面积变化及其影响因素
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

国家自然科学基金(42161020,U22A20454);青海省科技厅应用基础研究项目(2023-ZJ-943J)


Wetland area changes and influencing factors in Alpine Inland River Basin
Author:
Affiliation:

Fund Project:

The National Natural Science Foundation of China (General Program, Key Program, Major Research Plan)

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 文章评论
    摘要:

    高寒内陆河流域孕育的高寒湿地对气候变化敏感,极易受外部因素干扰并发生退化。及时准确的阐述高寒湿地面积变化特征及归因分析有助于提高兼具敏感性和脆弱性的高寒湿地资源保护和管理的科学性。青海湖流域位于青藏高原东北部,是全球变化的敏感区和青藏高原脆弱生态系统典型区,也是国际重要湿地分布区之一。基于GEE云平台和2000-2023年长时间序列Landsat遥感影像,采用随机森林分类方法对青海湖流域高寒湿地进行分类,分析其面积变化特征,最后结合相关分析和随机森林特征变量重要性排序方法探讨青海湖流域高寒湿地面积变化的影响因素。结果表明:(1)2000-2023年湿地分类的平均总体精度为88.45% (85.01%-92.63%),平均kappa系数为0.83(0.82-0.91),有效区分了湖泊、沼泽湿地和沼泽化草甸等高寒湿地类型。(2)研究期内青海湖流域湿地总面积增加了604.19 km2,其中沼泽湿地面积减少了228.21 km2,湖泊与沼泽化草甸面积分别增加了203.93 km2和628.47 km2。(3)受气候暖湿化影响,湿地呈现由干旱向湿润的转化趋势,主要体现为沼泽湿地与湖泊之间的转化、沼泽化草甸与草地之间的转化。24年内共有1101.44 km2草地转化为沼泽化草甸,2.93 km2湖泊转化为沼泽湿地,66.65 km2沼泽湿地转化为湖泊湿地。(4)青海湖流域不同海拔高度上因其气候、降水模式存在差异,致使主导不同湿地面积变化的气候因子不同。降水和季节性积雪是影响青海湖流域高寒湿地面积变化的主要因素。研究结果可为流域尺度高寒湿地的科学保护提供相关依据。

    Abstract:

    wetlands within alpine inland river basins are highly sensitive to climate fluctuations,readily affected by external disruptions,and inclined to degrade. Timely and precise delineations of changes in alpine wetland areas are vital for enhancing scientific conservation and management efforts. This helps address the sensitivity and vulnerability of alpine wetland resources. The Qinghai Lake Basin,sensitive to global changes,represents a quintessential area of delicate ecosystems on the Qinghai-Tibet Plateau and serves as a distribution zone for internationally significant wetlands. This study leveraged the Google Earth Engine (GEE) platform,employing a long-term dataset of Landsat remote sensing imagery spanning from 2000 to 2023. The random forest classification approach was applied to categorize alpine wetlands within the Qinghai Lake Basin,examining characteristics of their area alterations. Finally,combining correlation analysis and the random forest variable importance ranking method,factors influencing the area changes of alpine wetlands in the Qinghai Lake basin were investigated. The findings disclosed that (1) The mean overall accuracy of wetland classification from 2000 to 2023 was 88.45% (varying between 85.01% and 92.63%),accompanied by an average kappa coefficient of 0.83 (varying between 0.82 and 0.91). In the past,the classification accuracy of swamp meadow was relatively low,with average producer accuracy and average user accuracy at 77.99% and 86.74%,respectively. Lake classification had the highest accuracy,with average producer accuracy at 98.20% and user accuracy at 99.27%. Swamps registered an average producer accuracy of 86.03% and user accuracy of 86.66%,effectively discerning alpine wetland categories including lakes,swamps,and swamp meadows. (2) During the study period,the total wetland area in the Qinghai Lake Basin increased by 604.19 km2,with the swamp areas decreasing by 228.21 km2,while the lake and swamp meadow areas increased by 203.93 km2 and 628.47 km2,respectively. Among the three types of wetlands,swamp meadow showed the greatest variability in the past,exhibiting a fluctuating upward trend,increasing from 21.23% to 28.70% of the total wetland area. Swamp decreased from 6.87% to 2.85% of the total wetland area. The lake area initially decreased between 2003 and 2005,followed by a gradual increase,with a change of 4.65% over time.(3) Driven by increased warmth and precipitation,wetlands exhibited a shift from arid to humid states,primarily marked by transitions between swamps and lakes,as well as between swamp meadows and grasslands. Over 24 years,1101.44 km2 of grasslands converted to swamp meadow,2.93 km2 of lake converted to swamp,and 66.65 km2 of swamp converted to lake. (4) Attributable to variations in climate and precipitation patterns across varying elevations,distinct climatic elements govern the alterations in wetland areas within the Qinghai Lake Basin. In alpine regions,the swamp meadow showed a significant positive correlation with spring snow albedo; the area of lake affected by seasonal snow cover varied. precipitation and seasonal snow cover are the main factors influencing changes in high-altitude wetland areas. The results of this study can provide relevant basis for the scientific conservation and management of alpine wetlands at the basin scale.

    参考文献
    相似文献
    引证文献
引用本文

杨景云,金鑫,金彦香,陈克龙,谢慧春,李子昂,傅笛.高寒内陆河流域湿地面积变化及其影响因素.生态学报,2025,45(8):3684~3699

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数: