海岸沙丘形态对季风/台风的协同响应研究现状与展望  

Research status and prospect of the synergistic response of coastal dunes morphology to monsoon/typhoon

作　　者：杨林 Yang Lin(College of Tourism and Geography,Shaoguan University,Shaoguan 512005,Guangdong,China)

机构地区：[1]韶关学院旅游与地理学院,广东韶关512005

出　　处：《中国沙漠》2022年第1期108-113,共6页Journal of Desert Research

基　　金：国家自然科学基金项目(42101008);韶关学院校级科研项目(SY2018KJ01)。

摘　　要：海岸沙丘形态变化及其动力学过程是认识和研究海岸风沙地貌的基础。中国海岸沙丘受季风和台风共同驱动,但梳理总结海岸沙丘形态对季风/台风的响应研究、海岸沙丘形态-动力学过程研究及其技术和方法等发现,现有研究对中国海岸沙丘受季风/台风协同驱动的特点认识不足,对季风和台风的影响分别进行研究,与海岸沙丘形成与演化过程并不相符,季风和台风在沙丘形态发育与演变过程中的主次作用亦未知。据此现状,提出了当前开展国内海岸沙丘形态对季风/台风的协同响应研究紧迫性和亟需解决的问题。The morphological changes and dynamic process of coastal dunes are the basis for understanding and studying coastal aeolian landforms.Coastal dunes in South China are driven by monsoon and typhoon.However,through combing and summarizing the response of coastal dunes to monsoons/typhoons,coastal dunes morphology-dynamic process research and its technology and methods,it is found that current research on the characteristics of coastal sand dunes in China driven by the monsoon/typhoon synergy is insufficient,and the effects of monsoon and typhoon are studied separately,which are not consistent with the formation and evolution of coastal dunes.The primary and secondary effects of monsoons and typhoons in the development and evolution of dunes are also unknown.The urgency and urgent problems to be solved in the current research on the coordinated response of the coastal sand dune morphology to the monsoon/typhoon are put forward.

关 键 词：海岸沙丘 形态-动力学 季风 台风 

分 类 号：P931.3[天文地球—自然地理学]