论文

福建丹霞地貌旅游景区客流时间分布特性及其影响因素

展开
  • 1. 福建师范大学地理科学学院, 福建 福州 350007;
    2. 福建师范大学旅游学院, 福建 福州 350007

收稿日期: 2009-07-11

  修回日期: 2009-11-06

  网络出版日期: 2010-05-20

基金资助

福建省自然科学基金项目(2009J01209);福建省教育厅科技项目(JB08055)资助。

The Temporal Characteristics of Tourist Flows to Danxia Landform Scenic Spots in Fujian Province and Its Influence Factors

Expand
  • 1. College of Geographical Sciences and Tourism, Fujian Normal University, Fuzhou, Fujian, 350007;
    2. College of Tourism, Fujian Namal University, Fuzhou, Fujian, 350007

Received date: 2009-07-11

  Revised date: 2009-11-06

  Online published: 2010-05-20

摘要

地处闽西的武夷山、泰宁金湖、连城冠豸山、永安桃源洞等国家重点风景名胜区均属典型的丹霞地貌类型景区,距离较近,开展它们客流时间分布比较研究对各景区旅游业发展具有指导意义。运用小波分析、季节性强度指数、旅游气候舒适度模型等方法,对这4个旅游景区客流时间分布特性及其影响因素进行分析比较。结果表明,2001~2008年每个景区接待游客数量总体上是增加的,武夷山年游客数量最大,泰宁金湖景区客流年际波动辐度较大;武夷山景区客流年内变化曲线为"三峰三谷",泰宁金湖景区为"驼峰",冠豸山、桃源洞景区为"两高峰、两中峰、四低谷",泰宁金湖客流年内变化最大,冠豸山、桃源洞次之,武夷山最小;冠豸山和桃源洞景区客流月内波动要比武夷山、泰宁金湖景区大一些;连城冠豸山周内客流峰值分布在周日,其他景区客流峰值在周六,武夷山黄金周游客接待量最大。并对气候因素、社会因素、景区知名度、对外交通条件、旅游管理体制与管理水平等影响因素进行了分析。

本文引用格式

骆培聪, 张明锋 . 福建丹霞地貌旅游景区客流时间分布特性及其影响因素[J]. 地理科学, 2010 , 30(3) : 377 -383 . DOI: 10.13249/j.cnki.sgs.2010.03.377

Abstract

All the national key scenic spots of Wuyi Mountain, the Golden Lake of Taining, the Taoyuan Cave of Yong’an, and Guanzhai Mountain in Liancheng, belong to the typical Danxia landform. They are located in west Fujian Province with a short distance between each other. Therefore, it is of great significance to conduct a comparative study on the temporal distribution of tourist flows in the context of sustainable development of these four spots. Using methods such as wavelet analysis, seasonal intensity index, tourism climate comfort model, this paper analyzed and compared the temporal characteristics of tourist flows of the four spots and their influencing factors and obtains the following results: ① The amount of tourists of the four spots increased from 2001 to 2008; the number of tourists of Wuyi Mountain is the largest, and tourist flows to the Golden Lake in Taining is characterized by significant fluctuation between the years;②The seasonal curve of the tourist flow at Wuyi Mountain is characterized by "three peaks and three valleys", the seasonal curve of the tourist flow at the Golden Lake of Taining is characterized by "Camel back", and the seasonal curve of the tourist flow of Guanzhai Mountain and that of Taoyuan Cave of Yong’an are characterized by "two big peaks, two small peaks, and four valleys". The seasonal change of the tourist flow at the Golden Lake in Taining is the most obvious, followed by that of Taoyuan Cave,Guanzhai Mountain, and Wuyi Mountain;③ The fluctuations of the tourist flows within a month at both the Taoyuan Cave and Guanzhai Mountain were larger than that of Wuyi Mountain and the Golden Lake in Taining; ④While the peak of tourist flow of Guanzhai Mountain was on Sunday of the week, such peaks at other spots appears on Saturday, and the tourists number of Wuyi Mountain is the largest in golden weeks. The article also analyzes factors affecting the tourist flows, including climate, popularity, traffic conditions and management system and its standards of the above scenic spots.

参考文献

[1] 黄 进.中国丹霞地貌的分布[J].经济地理,1999,19(增刊):31~35.
[2] 黄 进.我对中国丹霞地貌的考察[J].经济地理,2003,23(增刊):200~223.
[3] 汪榕光,陈友飞,李祖光,等.福建丹霞地貌与旅游资源[J].经济地理,1994,14(增刊):111~116.
[4] 郑耀星.旅游资源评价与自然环境影响的关系——以福建省旅游资源特点为例[J].资源科学.2000,22(6):25~30.
[5] 赵西萍,王 磊.旅游目的地国际旅游需求预测方法综述[J].旅游学刊,1996,11(6):28~32.
[6] 孙根年.我国境外旅游本底趋势线的建立及科学意义[J].地理科学,1998,18(5):442~448.
[7] Cooper C P. Spatial and temporal patterns of tourist behaviour[J]. Regional Studies, 1981, 15 (5):359-371.
[8] Xia C, Zeephongsekul P, Arrowsmith C.Modelling spatio-temporal movement of tourists using finite Markov chains[J]. Mathematics and Computers in Simulation, 2009, 79(5):1544-1553.
[9] 张 红,李九全.桂林境外游客结构特征及时空动态模式研究[J].地理科学,2000,20(4):350~354.
[10] 牛亚菲,谢丽波,刘春凤.北京市旅游客流时空分布特征与调控对策[J].地理研究,2005,24(2):283~292.
[11] 刘宏盈,马耀峰.广东入境旅游流西向扩散时空动态演变研究[J].人文地理,2009,(4):124~128.
[12] 陆 林.山岳风景区旅游季节性研究——以安徽黄山为例[J].地理研究,1994,13(4):50~56.
[13] Lim C, McAleer M. A seasonal analysis of Malaysian tourist arrivals to Australia[J].Mathematics and Computers in Simulation, 1999, 48 (4-6):573-583.
[14] 李 想,黄震方.南京旅游客流时间分布特征分析[J].南京师大学报(自然科学版),2000,23(4):130~135.
[15] Hui T K,Yuen C C. A study in the seasonal variation of Japanese tourist arrivals in Singapore[J].Tourism Management, 2002, 23( 2): 127-131.
[16] 卢 松,陆 林,王 莉,等.古村落旅游客流时间分布特征及其影响因素研究——以世界文化遗产西递、宏村为例[J].地理科学,2004,24(2):250~256.
[17] 钟 静,张 捷,李东和,等.历史文化村镇旅游流季节性特征比较研究——以西递、周庄为例[J].人文地理, 2007, 22 (4):68~71.
[18] 颜 磊,许学工,章小平.九寨沟世界遗产地旅游流时间特征分析[J].北京大学学报(自然科学版),2009,45(1):171~177.
[19] 张 捷,都金康,周寅康,等.观光旅游地客流时间分布特性的比较研究[J].地理科学,1999,19(1):49~54.
[20] 汪德根,陆 林,刘昌雪,等.山岳型旅游地国内客流时空特性——以黄山、九华山为例[J].山地学报,2004,22(5):625~632.
[21] 陆 林,宣国富,章锦河,等.海滨型与山岳型旅游地客流季节性比较[J].地理学报,2002,57(6):731~740.
[22] 安 全,梁 川,刘 政.雅砻江中上游径流变化特性的小波分析[J].武汉大学学报(工学版),2008,41(3):20~24.
[23] 李双成,赵志强,高江波.基于空间小波变换的生态地理界线识别与定位[J].生态学报,2008,28(9):4313~4321.
[24] 保继刚,楚义芳,彭 华,等.旅游地理学[M].北京:高等教育出版社,1993:33~38.
[25] 罗晓玲,兰晓波,李岩瑛,等.人体舒适度指数预报体系研究[J].干旱区资源与环境,2004,18(8):59~62.
文章导航

/