請用此 Handle URI 來引用此文件:
http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/70926
完整後設資料紀錄
DC 欄位 | 值 | 語言 |
---|---|---|
dc.contributor.advisor | 沈聖峰(Sheng-Feng Shen) | |
dc.contributor.author | Ting-Chu Hsieh | en |
dc.contributor.author | 謝婷竹 | zh_TW |
dc.date.accessioned | 2021-06-17T04:44:11Z | - |
dc.date.available | 2023-08-07 | |
dc.date.copyright | 2018-08-07 | |
dc.date.issued | 2018 | |
dc.date.submitted | 2018-08-03 | |
dc.identifier.citation | Barton, K. (2009). MuMIn: multi-model inference, R package version 0.12. 0. http://r-forge. r-project. org/projects/mumin/.
Bates, D., Mächler, M., Bolker, B., & Walker, S. (2014). Fitting linear mixed-effects models using lme4. arXiv preprint arXiv:1406.5823. Beck-Johnson, L. M., Nelson, W. A., Paaijmans, K. P., Read, A. F., Thomas, M. B., & Bjornstad, O. N. (2017). The importance of temperature fluctuations in understanding mosquito population dynamics and malaria risk. Royal Society open science, 4(3), 160969. Beck, J., Liedtke, H. C., Widler, S., Altermatt, F., Loader, S. P., Hagmann, R., Lang, S., & Fiedler, K. (2016). Patterns or mechanisms? Bergmann’s and Rapoport’s rule in moths along an elevational gradient. Community Ecology, 17(2), 137-148. Bhutiyani, M. R., Kale, V. S., & Pawar, N. J. (2009). Climate change and the precipitation variations in the northwestern Himalaya: 1866-2006. International Journal of Climatology. Braganza, K., Karoly, D. J., & Arblaster, J. (2004). Diurnal temperature range as an index of global climate change during the twentieth century. Geophysical Research Letters, 31(13). Briga, M., & Verhulst, S. (2015). Large diurnal temperature range increases bird sensitivity to climate change. Scientific reports, 5. Burger, F., Brock, B., & Montecinos, A. (2018). Seasonal and elevational contrasts in temperature trends in Central Chile between 1979 and 2015. Global and Planetary Change, 162, 136-147. Chan, W., Chen, I., Colwell, R. K., Liu, W., Huang, C., & Shen, S. (2016). Seasonal and daily climate variation have opposite effects on species elevational range size. Science, 351(6280), 1437-1439. Compton, T. J., Rijkenberg, M. J., Drent, J., & Piersma, T. (2007). Thermal tolerance ranges and climate variability: a comparison between bivalves from differing climates. Journal of Experimental Marine Biology and Ecology, 352(1), 200-211. Dai, A., Trenberth, K. E., & Karl, T. R. (1999). Effects of clouds, soil moisture, precipitation, and water vapor on diurnal temperature range. Journal of Climate, 12(8), 2451-2473. Daly, C., Gibson, W. P., Taylor, G. H., Johnson, G. L., & Pasteris, P. (2002). A knowledge-based approach to the statistical mapping of climate. Climate Research, 22(2), 99-113. Easterling, D. R., Horton, B., Jones, P. D., Peterson, T. C., Karl, T. R., Parker, D. E., Salinger, M. J., Razuvayev, V., Plummer, N., & Jamason, P. (1997). Maximum and minimum temperature trends for the globe. Science, 277(5324), 364-367. Elsen, P. R., & Tingley, M. W. (2015). Global mountain topography and the fate of montane species under climate change. Nature Climate Change, 5(8), 772-776. Fleishman, E., Austin, G. T., & Weiss, A. D. (1998). An empirical test of Rapoport’s rule: elevational gradients in montane butterfly communities. Ecology, 79(7), 2482-2493. Fu, C., Hua, X., Li, J., Chang, Z., Pu, Z., & Chen, J. (2006). Elevational patterns of frog species richness and endemic richness in the Hengduan Mountains, China: geometric constraints, area and climate effects. Ecography, 29(6), 919-927. Gaston, K. J., & Chown, S. L. (1999). Elevation and climatic tolerance: a test using dung beetles. Oikos, 584-590. Geerts, B. (2003). Empirical estimation of the monthly-mean daily temperature range. Theoretical and Applied Climatology, 74(3), 145-165. Ghalambor, C. K., Huey, R. B., Martin, P. R., Tewksbury, J. J., & Wang, G. (2006). Are mountain passes higher in the tropics? Janzen's hypothesis revisited. Integrative and comparative biology, 46(1), 5-17. Gilchrist, G. W. (1995). Specialists and generalists in changing environments. I. Fitness landscapes of thermal sensitivity. The American Naturalist, 146(2), 252-270. Harris, I., Jones, P., Osborn, T., & Lister, D. (2014). Updated high‐resolution grids of monthly climatic observations–the CRU TS3. 10 Dataset. International Journal of Climatology, 34(3), 623-642. Hernandez-Barrera, S., Rodriguez-Puebla, C., & Challinor, A. (2016). Effects of diurnal temperature range and drought on wheat yield in Spain. Theoretical and Applied Climatology, 1-17. Jackson, L. S., & Forster, P. M. (2010). An empirical study of geographic and seasonal variations in diurnal temperature range. Journal of Climate, 23(12), 3205-3221. Jaeger, B. (2016). R2glmm: computes R squared for mixed (multilevel) models. R package version 0.1, 1. Janzen, D. H. (1967). Why mountain passes are higher in the tropics. The American Naturalist, 101(919), 233-249. Jones, P., & Briffa, K. (1992). Global surface air temperature variations during the twentieth century: Part 1, spatial, temporal and seasonal details. The Holocene, 2(2), 165-179. Jones, P. D., Lister, D. H., Osborn, T. J., Harpham, C., Salmon, M., & Morice, C. P. (2012). Hemispheric and large-scale land-surface air temperature variations: An extensive revision and an update to 2010. Journal of Geophysical Research: Atmospheres, 117(D5). Jungo, P., & Beniston, M. (2001). Changes in the anomalies of extreme temperature anomalies in the 20 th century at Swiss climatological stations located at different latitudes and altitudes. Theoretical and Applied Climatology, 69(1-2), 1-12. Karl, T. R., Knight, R. W., Gallo, K. P., Peterson, T. C., Jones, P. D., Kukla, G., Plummer, N., Razuvayev, V., Lindseay, J., & Charlson, R. J. (1993). A new perspective on recent global warming: asymmetric trends of daily maximum and minimum temperature. Bulletin of the American Meteorological Society, 74(6), 1007-1023. Karl, T. R., Kukla, G., & Gavin, J. (1984). Decreasing diurnal temperature range in the United States and Canada from 1941 through 1980. Journal of climate and applied meteorology, 23(11), 1489-1504. Kattel, D. B., & Yao, T. (2013). Recent temperature trends at mountain stations on the southern slope of the central Himalayas. Journal of earth system science, 122(1), 215-227. Kern, P., Cramp, R. L., & Franklin, C. E. (2015). Physiological responses of ectotherms to daily temperature variation. Journal of Experimental Biology, 218(19), 3068-3076. Kerr, J. T. (1999). Weak links:‘Rapoport's rule’and large‐scale species richness patterns. Global ecology and biogeography, 8(1), 47-54. Khaliq, I., Hof, C., Prinzinger, R., Bohning-Gaese, K., & Pfenninger, M. (2014). Global variation in thermal tolerances and vulnerability of endotherms to climate change. ProceedingS of the Royal Society B, 281(1789), 20141097. Kilpatrick, K., Podesta, G., & Evans, R. (2001). Overview of the NOAA/NASA advanced very high resolution radiometer Pathfinder algorithm for sea surface temperature and associated matchup database. Journal of Geophysical Research: Oceans, 106(C5), 9179-9197. Kim, J., Shin, J., Lim, Y.-H., Honda, Y., Hashizume, M., Guo, Y. L., Kan, H., Yi, S., & Kim, H. (2016). Comprehensive approach to understand the association between diurnal temperature range and mortality in East Asia. Science of the Total Environment, 539, 313-321. Kluge, J., Kessler, M., & Dunn, R. R. (2006). What drives elevational patterns of diversity? A test of geometric constraints, climate and species pool effects for pteridophytes on an elevational gradient in Costa Rica. Global ecology and biogeography, 15(4), 358-371. Kneis, D., Petzoldt, T., & Berendonk, T. U. (2017). An R-package to boost fitness and life expectancy of environmental models. Environmental Modelling & Software, 96, 123-127. Kriticos, D. J., Webber, B. L., Leriche, A., Ota, N., Macadam, I., Bathols, J., & Scott, J. K. (2012). CliMond: global high‐resolution historical and future scenario climate surfaces for bioclimatic modelling. Methods in Ecology and Evolution, 3(1), 53-64. Lagouarde, J. P., & Brunet, Y. (1993). A simple model for estimating the daily upward longwave surface radiation flux from NOAA-AVHRR data. International Journal of Remote Sensing, 14(5), 907-925. Legates, D. R., & Willmott, C. J. (1990). Mean seasonal and spatial variability in global surface air temperature. Theoretical and Applied Climatology, 41(1-2), 11-21. Li, Y., Li, X., Sandel, B., Blank, D., Liu, Z., Liu, X., & Yan, S. (2015). Climate and topography explain range sizes of terrestrial vertebrates. Nature Climate Change, 6(5), 498-502. Linacre, E. (1982). The effect of altitude on the daily range of temperature. International Journal of Climatology, 2(4), 375-382. Lindvall, J., & Svensson, G. (2015). The diurnal temperature range in the CMIP5 models. Climate Dynamics, 44(1-2), 405-421. Liu, X., Cheng, Z., Yan, L., & Yin, Z.-Y. (2009). Elevation dependency of recent and future minimum surface air temperature trends in the Tibetan Plateau and its surroundings. Global and Planetary Change, 68(3), 164-174. Lobell, D. B. (2007). Changes in diurnal temperature range and national cereal yields. Agricultural and forest meteorology, 145(3), 229-238. McCain, C. M. (2009). Vertebrate range sizes indicate that mountains may be 'higher' in the tropics. Ecol Lett, 12(6), 550-560. McCain, C. M., & Bracy Knight, K. (2013). Elevational Rapoport's rule is not pervasive on mountains. Global ecology and biogeography, 22(6), 750-759. Mumladze, L., Asanidze, Z., Walther, F., & Hausdorf, B. (2017). Beyond elevation: testing the climatic variability hypothesis vs. Rapoport’s rule in vascular plant and snail species in the Caucasus. Biological Journal of the Linnean Society, 121(4), 753-763. Pecl, G. T., Araújo, M. B., Bell, J. D., Blanchard, J., Bonebrake, T. C., Chen, I.-C., Clark, T. D., Colwell, R. K., Danielsen, F., & Evengård, B. (2017). Biodiversity redistribution under climate change: Impacts on ecosystems and human well-being. Science, 355(6332), eaai9214. Pintor, A. F., Schwarzkopf, L., & Krockenberger, A. K. (2015). Rapoport's Rule: Do climatic variability gradients shape range extent? Ecological Monographs, 85(4), 643-659. Pouteau, R., Rambal, S., Ratte, J.-P., Gogé, F., Joffre, R., & Winkel, T. (2011). Downscaling MODIS-derived maps using GIS and boosted regression trees: The case of frost occurrence over the arid Andean highlands of Bolivia. Remote Sensing of Environment, 115(1), 117-129. Price, T. D., Helbig, A. J., & Richman, A. D. (1997). Evolution of breeding distributions in the Old World leaf warblers (genus Phylloscopus). Evolution, 51(2), 552-561. Rahbek, C. (1997). The relationship among area, elevation, and regional species richness in neotropical birds. The American Naturalist, 149(5), 875-902. Rangwala, I., & Miller, J. R. (2012). Climate change in mountains: a review of elevation-dependent warming and its possible causes. Climatic Change, 114(3), 527-547. Rolland, C. (2003). Spatial and seasonal variations of air temperature lapse rates in Alpine regions. Journal of Climate, 16(7), 1032-1046. Stevens, G. C. (1989). The latitudinal gradient in geographical range: how so many species coexist in the tropics. The American Naturalist, 133(2), 240-256. Stevens, G. C. (1992). The elevational gradient in altitudinal range: an extension of Rapoport's latitudinal rule to altitude. The American Naturalist, 140(6), 893-911. Stevens, G. C. (1996). Extending Rapoport's rule to Pacific marine fishes. Journal of Biogeography, 23(2), 149-154. Telwala, Y., Brook, B. W., Manish, K., & Pandit, M. K. (2013). Climate-induced elevational range shifts and increase in plant species richness in a Himalayan biodiversity epicentre. PLoS One, 8(2), e57103. Thorne, P., Donat, M., Dunn, R., Williams, C., Alexander, L., Caesar, J., Durre, I., Harris, I., Hausfather, Z., & Jones, P. (2016). Reassessing changes in diurnal temperature range: Intercomparison and evaluation of existing global data set estimates. Journal of Geophysical Research: Atmospheres, 121(10), 5138-5158. Van De Kerchove, R., Lhermitte, S., Veraverbeke, S., & Goossens, R. (2013). Spatio-temporal variability in remotely sensed land surface temperature, and its relationship with physiographic variables in the Russian Altay Mountains. International Journal of Applied Earth Observation and Geoinformation, 20, 4-19. Vangansbeke, D., Audenaert, J., Nguyen, D. T., Verhoeven, R., Gobin, B., Tirry, L., & De Clercq, P. (2015). Diurnal temperature variations affect development of a herbivorous arthropod pest and its predators. PLoS One, 10(4), e0124898. Wang, G.-y., Zhao, M.-f., Kang, M.-y., Xing, K.-x., Wang, Y.-h., Xue, F., & Chen, C. (2017). Diurnal and seasonal variation of the elevation gradient of air temperature in the northern flank of the western Qinling Mountain range, China. Journal of Mountain Science, 14(1), 94-105. Wang, G., & Dillon, M. E. (2014). Recent geographic convergence in diurnal and annual temperature cycling flattens global thermal profiles. Nature Climate Change, 4(11), 988-992. Whitton, F. J., Purvis, A., Orme, C. D. L., & Olalla‐Tárraga, M. Á. (2012). Understanding global patterns in amphibian geographic range size: does Rapoport rule? Global ecology and biogeography, 21(2), 179-190. Wild, M. (2009). How well do IPCC‐AR4/CMIP3 climate models simulate global dimming/brightening and twentieth‐century daytime and nighttime warming? Journal of Geophysical Research: Atmospheres, 114(D10). Zhou, L., Dai, A., Dai, Y., Vose, R. S., Zou, C.-Z., Tian, Y., & Chen, H. (2009). Spatial dependence of diurnal temperature range trends on precipitation from 1950 to 2004. Climate Dynamics, 32(2), 429-440. | |
dc.identifier.uri | http://tdr.lib.ntu.edu.tw/jspui/handle/123456789/70926 | - |
dc.description.abstract | 近年關於氣候變遷的相關討論由大氣領域,逐漸擴展至公共衛生、農業與生態等相關學門,其中,氣候變遷對生物分布範圍(species range size)變化之潛在影響,是生態領域的新興議題之一。氣候變異假說(climatic variability hypothesis)即描述環境因子如何影響物種分布:氣候變異度大的區域,較適合溫度容忍範圍(thermal tolerance)與生物分布範圍廣的物種生存。Stevens以此假說解釋生物分布範圍隨緯度或海拔增加而變廣之現象,即Rapoport’s rule,但過去以來,關於Rapoport’s rule的相關研究結果仍有爭議,可能與缺乏實際分析日溫差與年溫差等氣候變異度沿海拔變化相關。因此本文希望透過了解全球網格資料的山區日溫差與年溫差變化,以及各別山系的日溫差與年溫差對生物分布範圍之影響,以氣候變異度假說解釋山區生物分布範圍變化。全球日溫差、年溫差與降水等網格資料來自Climatic Research Unit (CRU) TS3.10.01資料庫的1901-2000年間資料,海拔網格資料取自Digital Elevation Model (DEM),距海遠近資料取自National Aeronautics and Space Administration (NASA),並使用「影響面積」考量地表向上長波輻射對地表溫度之影響。所有資料按Natural Earth所定義的山系範圍,選取全球共182座山系,生物分布範圍資料取自相關發表文獻,透過R以單因子與多因子簡單線性模式,以及混和效果模式(mixed- effect model)分析。全球網格資料結果顯示,海拔對部分山區的日溫差或年溫差沒有顯著影響,但有顯著影響的山系,多座落於中高緯度與較內陸地區,各別山系結果僅部份支持氣候變異度假說,但辨別海拔對山區日溫差與年溫差影響顯著與否,以及區分不同海拔段分析仍有助於討論日溫差與年溫差對生物分布範圍影響,此外,本文最後也提出鑑別海拔是否影響山區日溫差與年溫差之參考標準。上述結果除作為探討氣候變異度對山區生物分布範圍影響之背景知識外,也能用於評估未來全球暖化將對山區生物產生哪些衝擊,以及應用於人體健康與農業等其他領域。 | zh_TW |
dc.description.abstract | Climatic variability hypothesis, which predicts the correlation between range sizes of species and the variation of climatic parameters experienced by these species, is used to explain Rapoport’s rule, an increase of elevational range size with higher elevations. However, the generality of the rule has been challenged and evidence towards explanatory mechanisms has been equivocal. The aims of our study are to analyze the pattern of diurnal and seasonal temperature range (DTR and STR) in global mountains and investigate its’ relationship to species range sizes. The meteorological data for mountain DTR were extracted from the Climatic Research Unit (CRU) TS3.10.01 dataset, and the geographical data for elevation and distance to coast were obtained from Digital Elevation Model (DEM) and National Aeronautics and Space Administration (NASA), respectively. All the information of mountain ranges is from the website, Natural Earth. Simple linear regression and mixed-effect model in R program was used to examine on mountain climatic variability and its related factors. Besides, we also tested for relationships between mountain climatic variability and species range sizes across 31 mountains worldwide. Our results indicated that the trends of DTR and STR in some global mountains were weakly influenced by elevation, yet the other mountains, which mostly located at inland or higher latitudes, were significantly affected by elevation. Although only a few results suggested a positive relationship between mountain climatic variability and species range sizes, we found that sorting species range sizes by elevation and investigating the trend of local climatic variability can enhance our ability to understand the distribution of biodiversity. | en |
dc.description.provenance | Made available in DSpace on 2021-06-17T04:44:11Z (GMT). No. of bitstreams: 1 ntu-107-R05247002-1.pdf: 4294628 bytes, checksum: 58b44b59d706fb2115f4d77c01ca49da (MD5) Previous issue date: 2018 | en |
dc.description.tableofcontents | 誌謝 I
摘要 II Abstract III 目錄 IV 圖目錄 V 表目錄 V 壹、前言 1 貳、材料與方法 4 一. 全球山區日溫差與年溫差 4 二. 日溫差與年溫差對生物分布範圍關係 5 參、分析方法與結果 7 一. 全球山區日溫差與年溫差變化 7 1. 山區日溫差與年溫差沿海拔變化 7 2. 山區日溫差與年溫差的相關因子分析 7 2.1. 分析方法 7 2.2. 山區日溫差與年溫差變化 8 2.3. 海拔顯著影響山系的地理特性 9 2.4. 判別海拔對山區日溫差或年溫差影響之參考標準 10 二. 各別山區日溫差與年溫差對生物分布範圍影響 11 1. 分析方法 11 2. 環境溫度因子與生物分布範圍關係 12 3. 不同海拔之環境溫度因子與生物分布範圍關係 13 4. 鑑別海拔對山區對日溫差或年溫差影響 13 肆、討論 15 伍、參考文獻 19 | |
dc.language.iso | zh-TW | |
dc.title | 全球山區氣候變異度及其對生物分布範圍影響 | zh_TW |
dc.title | Climatic Variability in Global Mountain Areas and Its Impacts on Species Range Size | en |
dc.type | Thesis | |
dc.date.schoolyear | 106-2 | |
dc.description.degree | 碩士 | |
dc.contributor.coadvisor | 羅敏輝(Min-Hui Lo) | |
dc.contributor.oralexamcommittee | 李培芬,黃倬英,陳一菁 | |
dc.subject.keyword | 日溫差,年溫差,氣候變異度假說,生物分布範圍, | zh_TW |
dc.subject.keyword | diurnal temperature range,seasonal temperature range,climatic variability hypothesis,species range size, | en |
dc.relation.page | 51 | |
dc.identifier.doi | 10.6342/NTU201802437 | |
dc.rights.note | 有償授權 | |
dc.date.accepted | 2018-08-03 | |
dc.contributor.author-college | 理學院 | zh_TW |
dc.contributor.author-dept | 氣候變遷與永續發展國際學位學程 | zh_TW |
顯示於系所單位: | 氣候變遷與永續發展國際學位學程(含碩士班、博士班) |
文件中的檔案:
檔案 | 大小 | 格式 | |
---|---|---|---|
ntu-107-1.pdf 目前未授權公開取用 | 4.19 MB | Adobe PDF |
系統中的文件,除了特別指名其著作權條款之外,均受到著作權保護,並且保留所有的權利。