[1] |
Sheppard P R. Overcoming extraneous wood color variation during low-magnification reflected-light image analysis of conifer tree rings[J]. Wood and fiber science:journal of the Society of Wood Science and Technology, 1999,31(2):106-115.
|
[2] |
Schweingruber F H, Fritts H C, Braker O U, et al. The X-ray technique as applied to dendrochronology[J]. Tree-ring Bulletin, 1978,38:61-91.
|
[3] |
Mccarroll D, Pettigrew E, Luckman A. Blue Reflectance Provides a Surrogate for Latewood Density of High-latitude Pine Tree Rings[J]. Arctic Antarctic and Alpine Research, 2002,34(4):450-453.
doi: 10.1080/15230430.2002.12003516
|
[4] |
Sheppard P R, Alex W. An advancement in removing extraneous color from wood for low-magnification reflected-light image analysis of conifer tree rings[J]. Wood & Fiberence, 2007,39(1):173-183.
|
[5] |
Wilson R, Rohit R, Rydval M, et al. Blue Intensity for dendroclimatology:The BC blues:A case study from British Columbia,Canada[J]. The Holocene, 2014,8:1-11.
doi: 10.1191/095968398670905088
|
[6] |
Wilson R, Wilson D, Rydval M, et al. Facilitating tree-ring dating of historic conifer timbers using Blue Intensity[J]. Journal of Archaeological Science, 2016,78:99-111.
doi: 10.1016/j.jas.2016.11.011
|
[7] |
Rydval M, Larsson L, Laura M, et al. Blue intensity for dendroclimatolog:Should we have the blues?Experiments from Scotland[J]. Dendrochronologia, 2014,32(3):191-204.
doi: 10.1016/j.dendro.2014.04.003
|
[8] |
Mauricio F, Björklund J, Seftigen K, et al. A comparison between Tree-Ring Width and Blue Intensity high and low frequency signals from Pinus sylvestris L.from the Central and Northern Scandinavian Mountains[J]. TRACE-Tree Rings in Archaeology,Climatology and Ecology, 2016,14:38-43.
|
[9] |
Campbell R, McCarroll D, Neil J L, et al. Blue intensity in Pinus sylvestris tree-rings:developing a new palaeoclimate proxy[J]. The Holocene, 2007,17(6):821-828.
doi: 10.1177/0959683607080523
|
[10] |
Babst F, Frank D, Büntgen U, et al. Effect of sample preparation and scanning resolution on the Blue Reflectance of Picea abies[J]. TRACE-Tree Rings in Archeology,Climatology and Ecology, 2009,7:189-195.
|
[11] |
Björklund J A, Gunnarson B E, Seftigen K, et al. Blue intensity and density from northern Fennoscandian tree rings,exploring the potential to improve summer temperature reconstructions with earlywood information[J]. Climate of the Past, 2014,10(2):877-885.
doi: 10.5194/cp-10-877-2014
|
[12] |
Björklund J A, Gunnarson B E, Seftigen K, et al. Using adjusted Blue Intensity data to attain high-quality summer temperature information:A case study from Central Scandinavia[J]. The Holocene, 2015,25(3):547-556.
doi: 10.1177/0959683614562434
|
[13] |
Mccarroll D, Mervi T, Campbell R, et al. A critical evaluation of multi-proxy dendroclimatology in northern Finland[J]. Journal of Quaternary Science, 2011,26(1):7-14.
doi: 10.1002/jqs.1408
|
[14] |
Österreicher A, Weber G, Leuenberger M, et al. Exploring blue intensity-comparison of blue intensity and MXD data from Alpine spruce trees[J]. TRACE-Tree Rings in Archaeology,Climatology and Ecology, 2015,13:56-61.
|
[15] |
Rydval M, Gunnarson B E, Loader N J, et al. Spatial reconstruction of Scottish summer temperatures from tree rings[J]. International Journal of Climatology, 2016.
doi: 10.1002/joc.4326
pmid: 27478303
|
[16] |
Dolgova E. June-September temperature reconstruction in the Northern Caucasus based on blue intensity data[J]. Dendrochronologia, 2016,39:17-23.
doi: 10.1016/j.dendro.2016.03.002
|
[17] |
Rydval M, Neil J L, Björn E G, et al. Reconstructing 800 years of summer temperatures in Scotland from tree rings[J]. Climate Dynamics, 2017,49(9):3478-3486.
|
[18] |
Fuentes M, Riikka S, Jesper B, et al. A 970-year-long summer temperature reconstruction from Rogen,west-central Sweden,based on blue intensity from tree rings[J]. The Holocene, 2017,28(2):1-13.
|
[19] |
Wilson R, Rosanne D, Laia A, et al. Experiments based on blue intensity for reconstructing North Pacific temperatures along the Gulf of Alaska[J]. Climate of the Past, 2017,13(8):1007-1022.
doi: 10.5194/cp-13-1007-2017
|
[20] |
Babst F, Wright W E, Szejner P, et al. Blue intensity parameters derived from Ponderosa pine tree rings characterize intra-annual density fluctuations and reveal seasonally divergent water limitations[J]. Trees, 2016,30(4):1403-1415.
doi: 10.1007/s00468-016-1377-6
|
[21] |
Buckley B M, Kyle G H, Kevin L G, et al. Blue intensity from a tropical conifer’s annual rings for climate reconstruction:An ecophysiological perspective[J]. Dendrochronologia, 2018,50:10-22.
doi: 10.1016/j.dendro.2018.04.003
|
[22] |
Arbellay E, Ingrid J, Raphaёl D C, et al. Tree-ring proxies of larch bud moth defoliation:latewood width and blue intensity are more precise than tree-ring width[J]. Tree Physiology, 2018,38:1237-1245.
doi: 10.1093/treephys/tpy057
pmid: 29788327
|
[23] |
黎韦水, 符韵林. 木材心材形成原因和机理研究进展[J]. 陕西林业科技, 2017(6):78-83.
|
[24] |
吴祥定. 树木年轮与气候变化[M]. 北京: 气象出版社, 1990.
|
[25] |
Li Minxiong, Okada N, Fujiwara T, et al. The dendrochronological potential of ten species in the Three Gorges Reservoir region of China[J]. IAWA Journal, 2000,21(2):181-196.
doi: 10.1163/22941932-90000244
|
[26] |
梁先娥. 基于Resistograph数据树木年轮对环境变化的响应[D]. 南京:南京林业大学, 2017.
|
[27] |
段建平. 树木年轮密度研究进展[J]. 第四纪研究, 2015,35(5):1271-1282.
doi: 10.11928/j.issn.1001-7410.2015.05.23
|