Spatial-temporal distribution of mountain-climate tourism resources in Lin’an, China

WANG Guoxin; YANG Xiaona; SU Fei

doi:10.11833/j.issn.2095-0756.2015.02.019

Volume 32 Issue 2

Mar. 2015

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WANG Guoxin, YANG Xiaona, SU Fei. Spatial-temporal distribution of mountain-climate tourism resources in Lin’an, China[J]. Journal of Zhejiang A&F University, 2015, 32(2): 298-307. doi: 10.11833/j.issn.2095-0756.2015.02.019

Citation:

WANG Guoxin, YANG Xiaona, SU Fei. Spatial-temporal distribution of mountain-climate tourism resources in Lin’an, China[J]. Journal of Zhejiang A&F University, 2015, 32(2): 298-307. doi: 10.11833/j.issn.2095-0756.2015.02.019

Spatial-temporal distribution of mountain-climate tourism resources in Lin’an, China

doi: 10.11833/j.issn.2095-0756.2015.02.019

1.
School of Tourism and City Administation, Zhejiang Gongshang University, Hangzhou 310018, Zhejiang, China

Received Date: 2014-07-02
Rev Recd Date: 2014-11-10
Publish Date: 2015-04-20

Abstract

Climatic data representing Linan City in Zhejiang Province was collected in 2012 from 15 meteorological stations. Data was analyzed and evaluated for spatial and temporal distribution characteristics of mountain-climate tourism resources using temperature humidity index （THI）, wind effect index （K）, lapse-rate of air temperature, and a high pressure equation. Then using a spatial overlay classification from GIS, the spatial and temporal distribution characteristics of mountain-climate resources were determined. Results showed that 1） for a mountain climate the most comfortable time for tourist rest and recreation was from April to June and September to October at an altitude of 800－1 600 m. Meanwhile, July and August were relatively hot, so tourists could escape the heat at altitudes of 975－1 787 m for south facing slopes and 1 196－1 787 m for north facing slopes. November to March was the cold-winter-months period and was more suitable for skiing at altitudes of 621－1 787 m for north-facing slopes and 754－1 787 m for south-facing slopes. 2） Considering spatial distribution, tourism resources for the mountain-climate in Linan were mainly distributed over the middle and lower mountain areas, such as Yaotou, Tianmu, and Daming Mountains. 3）The spatial overlay classification from GIS showed no obvious mountain-climate characteristics in Linan below 621 meters. In a word, it will be convenient for us to emphasize the elevation factor and take advantage of its superior characteristics in the development process of mountain-climate resources. ［Ch, 6 fig. 4 tab. 33 ref.］
- mountain climate,
- climate comfort index,
- lapse rate,
- spatial-temporal distribution,
- Lin’an City

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通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

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Spatial-temporal distribution of mountain-climate tourism resources in Lin’an, China

1. School of Tourism and City Administation, Zhejiang Gongshang University, Hangzhou 310018, Zhejiang, China

Received Date: 2014-07-02

Rev Recd Date: 2014-11-10

Publish Date: 2015-04-20

Key words:

Abstract: Climatic data representing Linan City in Zhejiang Province was collected in 2012 from 15 meteorological stations. Data was analyzed and evaluated for spatial and temporal distribution characteristics of mountain-climate tourism resources using temperature humidity index （THI）, wind effect index （K）, lapse-rate of air temperature, and a high pressure equation. Then using a spatial overlay classification from GIS, the spatial and temporal distribution characteristics of mountain-climate resources were determined. Results showed that 1） for a mountain climate the most comfortable time for tourist rest and recreation was from April to June and September to October at an altitude of 800－1 600 m. Meanwhile, July and August were relatively hot, so tourists could escape the heat at altitudes of 975－1 787 m for south facing slopes and 1 196－1 787 m for north facing slopes. November to March was the cold-winter-months period and was more suitable for skiing at altitudes of 621－1 787 m for north-facing slopes and 754－1 787 m for south-facing slopes. 2） Considering spatial distribution, tourism resources for the mountain-climate in Linan were mainly distributed over the middle and lower mountain areas, such as Yaotou, Tianmu, and Daming Mountains. 3）The spatial overlay classification from GIS showed no obvious mountain-climate characteristics in Linan below 621 meters. In a word, it will be convenient for us to emphasize the elevation factor and take advantage of its superior characteristics in the development process of mountain-climate resources. ［Ch, 6 fig. 4 tab. 33 ref.］

Spatial-temporal distribution of mountain-climate tourism resources in Lin’an, China

doi: 10.11833/j.issn.2095-0756.2015.02.019

Abstract

References

Proportional views

通讯作者: 陈斌, bchen63@163.com

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