TEL:886-2-2367-8532
FAX:886-2-2368-6732

Full-text available
   < Previous vol/No | Next vol/No >
Vol.53, No.4, PP.221-290
Content:   PDF( 0.73MB )

Editorial Scope and Editorial Board:  PDF( 0MB )

1
Downstream Scour Pits to Protect Open Check Dams
53(4):221-230
Hsun-Chuan Chan[1] Chun-Mei Chen[2] Meng-Chyung Shieh[2] Chien-Hui Chang[1]
* Corresponding Author. E-mail : hcchan@ nchu.edu.tw
Show preview   |   PDF( 10.86MB )   |  
2
Effects of Landslide Geomorphological Evolution on Subwatersheds: A Case Study in the Ailiao River Watershed
53(4):231-241
Cheng-Yi Lin Chun-Hung Wu
* Corresponding Author. E-mail : chhuwu@fcu.edu.tw
Show preview   |   PDF( 11.08MB )   |  
3
Study on the Influence of Vegetation Cover on Urban Air Temperature in the Taipei Botanical Garden
53(4):242-251
Shiang-Yue Lu[1] Shao-Wei Wu[2] Ming-Yuan Sun[3*]
* Corresponding Author. E-mail : smy@tfri.gov.tw
Show preview   |   PDF( 10.34MB )   |  
Study on the Influence of Vegetation Cover on Urban Air Temperature in the Taipei Botanical Garden
Close
Shiang-Yue Lu[1] Shao-Wei Wu[2] Ming-Yuan Sun[3*]

Abstract
The influence of vegetation cover on air temperatures was received more concerning recently. Air temperatures of above, under canopy and top of a concrete pavement building have been monitored for investigating the effects of tree canopy on air temperature. Results indicated that the yearly temperature difference between above and under canopy is about 0.42℃ and monthly highest temperature difference can be up to 0.93℃ during the summer season. The difference temperatures between above and under canopy showed no significant difference when temperature of above canopy below 27.2℃. The yearly difference temperatures between top of cement paved building and above canopy were 0.55℃ and showed no significant difference when the above canopy temperature below 24.3℃.
This study also used the Landsat-8 thermal images to estimate air temperatures of the entire Taipei metropolitan area through converting infrared wavelength to radiation intensity and calculating brightness temperature (TB). The obtained air temperature distribution map showed that the heat island effects can cause temperature of the urban area of Taipei city reaching up to 5.0 °C and temperature above vegetated zones showed a relatively lower temperature. These results also proved that vegetation coverages have a cooling effect to mitigate the effect of urban heat island (UHI) and provide a better understanding of the effects of vegetation cover on land surface temperature in the Taipei metropolitan area.
Key Words: air temperature, urban heat island effects, brightness temperature, thermal images
〔1〕Division of Watershed Management, Taiwan Forestry Research Institute
〔2〕Department of Soil and Water Conservation, National Chung Hsing University
〔3〕Liukuei Research Center, Taiwan Forestry Research Institute
* Corresponding Author. E-mail : smy@tfri.gov.tw
Received: 2021/09/22
Revised: 2021/11/18
Accepted: 2022/01/21
4
Effectiveness of Energy Dissipation Downstream of the Shih-Gang Dam by Hydraulic Model
53(4):264-272
Wei-Ming Wong
* Corresponding Author. E-mail : ming@wrap.gov.tw
Show preview   |   PDF( 69.38MB )   |  
5
Evolution of Landslide and Sediment Runoff in the Catchment of the Tsengwen Reservoir
53(4):273-284
Yu-Shiu Chen[1]* Wei-Lin Lee[2] Chien-Yang Lin[1] Yu-Lun Tsai[1] Shih-Hsun Lin[3]
* Corresponding Author. E-mail : yushiu.chen@dprc.ncku.edu.tw
Show preview   |   PDF( 53.24MB )   |  
   Copyright © 2011 Chinese Soil And Water Conservation Society   MAP    
Address:2FL, No.8, Lane 113, Xiamen St., Zhongzheng Dist., Taipei City 100, Taiwan (R.O.C.)