青藏高原全新世降水序列的集成重建

doi:10.11820/dlkxjz.2012.09.001

地理科学进展 ›› 2012, Vol. 31 ›› Issue (9): 1117-1123.doi: 10.11820/dlkxjz.2012.09.001

• 水文与气象过程 • 下一篇

青藏高原全新世降水序列的集成重建

侯光良, 鄂崇毅, 肖景义

青海师范大学青藏高原资源与环境教育部重点实验室, 西宁810008

收稿日期:2012-04-01 修回日期:2012-06-01 出版日期:2012-09-25 发布日期:2012-09-25
作者简介:侯光良(1972-),男,青海省人,教授,主要从事环境演变研究。E-mail:hgl20@163.com
基金资助:
国家自然科学基金项目(41161018);教育部人文社会科学研究青年基金项目(10YJCZH041);青海科技厅青年基金项目(2011-Z-926Q);青海师范大学昆仑学者经费项目。

Synthetical Reconstruction of the Precipitation Series of the Qinghai-Tibet Plateau during the Holocene

HOU Guangliang, E Chongyi, XIAO Jingyi

Key Laboratory of Qinghai-Tibetan Plateau Environment and Resource (MOE), School of Life and Geographic Science, Qinghai Normal University, Xining 810008, China

Received:2012-04-01 Revised:2012-06-01 Online:2012-09-25 Published:2012-09-25

摘要/Abstract

摘要： 青藏高原全新世降水变化对于过去全球变化研究有重要意义。在过去全球变化研究中, 大尺度区域降水序列重建缺乏可行、有效的方法, 本文以青藏高原作为研究区, 构建了分区古降水空间模拟－多区面积加权的集成方法, 重建全新世青藏高原降水序列。本研究以孢粉为环境证据, 选取有空间代表性的10 条由孢粉重建的高原样点降水序列, 获得716 条具有年代的定量降水记录, 建立全新世古降水记录数据集。借助GIS分析, 基于现代高原降水空间分布的地理因子模拟, 并与古降水记录相集成, 定量重建了高原全新世200 年分辨率的降水序列。结果显示:早全新世高原降水迅速增多, 并在9.0 kaBP达到极大值500 mm, 较现代高170 mm;9.0~5.6 kaBP是旺盛的湿润期, 降水总体比现代高出80 mm, 但呈现明显的下降趋势;5.6 kaBP以来降水减少, 降水与现代相当, 但波动幅度较小;集成序列与其他高低分辨率环境记录有很好的可比性, 说明集成序列有很好的代表性和一定的准确性。

关键词: 集成重建, 降水, 青藏高原, 全新世

Abstract: The precipitation change over the Qinghai-Tibet Plateau in Holocene is of great importance to the study of global change in the past. There is a lack of practical and effective methods to reconstruct precipitation in a large-scale region in the previous studies on global change, and in order to solve this problem, this study takes the Qinghai-Tibet Plateau as the research area and combines the method of partitioned space simulation of ancient precipitation and multi-area weighted method for the purpose of reconstructing the precipitation series of Qinghai-Tibet Plateau in Holocene. As the vegetation variation of Qinghai-Tibet Plateau can well reflect the precipitation change, this study mainly takes pollen as the circumstantial evidence, selects ten pollen reconstructed precipitation series of sampling points on the plateau, acquires 716 signaled quantitative precipitation records and reconstructs the precipitation series of the plateau in Holocene. With the help of GIS analysis, based on the geographical simulation of spatial distribution of modern plateau precipitation, and integrated with the ancient precipitation records, this paper quantitatively reconstructed the 200-resolution precipitation series of the plateau during the Holocene. The results indicated that during the Holocene the precipitation went up rapidly, reaching a peak of 500 mm at 9 ka BP, 170 mm more than that in modern times. The period 9-5.6 ka BP was a moist period with the total precipitation 80 mm more than that at present. However it showed a downward trend. Since 5.6 ka BP the precipitation went down compared with the present time with small fluctuation. Synthetic series are comparable to the other records in a high or low resolution, which means synthetic series are representative and accurate.

Key words: Holocene, precipitation, Qinghai-Tibet Plateau, synthesis reconstruction

侯光良, 鄂崇毅, 肖景义. 青藏高原全新世降水序列的集成重建[J]. 地理科学进展, 2012, 31(9): 1117-1123.

HOU Guangliang, E Chongyi, XIAO Jingyi. Synthetical Reconstruction of the Precipitation Series of the Qinghai-Tibet Plateau during the Holocene[J]. PROGRESS IN GEOGRAPHY, 2012, 31(9): 1117-1123.

参考文献

[1] 莫申国, 张百平, 程维明, 等. 青藏高原的主要环境效应. 地理科学进展, 2004, 23(2): 88-96.

[2] Kutzbach J E, Guetter P J, Ruddiman W F, et al. The sensitivityof climate to late Cenozoic uplift in southern Asiaand the American west: Numerical experiments. Journalof Geophysical Research, 1989, 94(3): 18393-18407.

[3] An Z S, Kutzbach J E, Prell W L, et al. Evolution ofAsian monsoons and phased uplift of the Himalayan-Tibetanplateau since late Miocene times. Nature, 2001, 411(18): 62-66.

[4] Prell W L, Kutzbach J E. Sensitivity of the Indian monsoonto forcing parameters and implications for its evolution.Nature, 1992, 360(10): 647-652.

[5] Bradley R S, Alverson T R, Pedersen F. Challenges of achanging earth: Past perspectives, future concerns//AlersonK R. Bradley T S, Pedersen F. Paleoclimate, GlobalChange and the Future. Berlin: Springer Verlag, 2003:163-167.

[6] COHMAP Members. Climatic changes of the last 18,000years: Observation and model simulations. Science, 1988,241(6): 1043-1052.

[7] 张家诚, 林之光. 中国气候. 上海: 上海科学技术出版社, 1985: 467-483.

[8] Herzschuh U, Kramer A, Mischke S, et al. Quantitativeclimate and vegetation trends since the late glacial on thenortheastern Tibetan Plateau deduced from Koucha Lakepollen spectra. Quaternary Research, 2009, 71(4):162-171.

[9] Herzschuh U, Birks H B, Mischke S, et al. A modern pollen-climate calibration set based on lake sediments fromthe Tibetan Plateau and its application to a Late Quaternarypollen record from the Qilian Mountains. Journal ofBiogeography, 2010, 37(1): 752-766.

[10] Wischnewski J, Mischke S, Wang Yongbo, et al. Reconstructingclimate variability on the northeastern Tibetanplateau since the last Lateglacial: A multi-proxy, dual-siteapproach comparing terrestrial and aquatic signals. QuaternaryScience Reviews, 2011, 30(4): 82-97.

[11] Tang L Y, Shen C M, Li C H, et al. Pollen-inferred vegetationand environmental changes in the central Tibetan Plateausince 8200 yr BP. Sci China Ser D: Earth Sci, 2009,doi: 10.1007/s11430-009-0080-5.

[12] 唐领余, 沈才明, Liu K M, 等. 南亚古季风的演变:西藏新的高分辨率古气候记录. 科学通报, 1999, 44(18):2004-2007.

[13] Shen C M, Liu K M, Tang L Y, et al. Quantitative relationshipsbetween modern pollen rain and climate in theTibetan Plateau. Review of Palaeobotany and Palynology,2006, 140(5): 61-77.

[14] Lu H Y, Wu N Q, Liu K M, et al. Modern pollen distributionsin Qinghai-Tibetan Plateau and the development oftransfer functions for reconstructing Holocene environmentalchanges. Quaternary Science Reviews, 2011, 30(3): 947-966.

[15] 葛全胜, 陈泮勤, 张雪芹. 全球变化的集成研究. 地球科学进展, 2000, 15(4): 461-466.

[16] 张兰生, 方修琦, 任国玉. 全球变化. 北京: 高等教育出版社, 2000.

[17] 鲁春霞, 王菱, 谢高地, 等. 青藏高原降水的梯度效应及其空间分布模拟. 山地学报, 2007, 25(6): 655-663.

[18] 林之光. 地形降水气候学. 北京: 科学出版社, 1995:6-45.

[19] 戴加洗. 青藏高原气候. 北京: 气象出版社, 1990: 51-184.

[20] 杜军, 马玉才. 西藏高原降水变化趋势的气候分析. 地理学报, 2004, 29(3): 375-382.

[21] Campo E V, Cour P, Hang S X. Holocene environmentalchanges in Bangong Co basin (Western Tibet). Part 2:The pollen record. Palaeogeography, Palaeoclimatology,Palaeoecology,1996, 120(5): 49-63.

[22] Campo E V, Gasse F. Pollen and diatom-inferred climaticand hydrological changes in Sumxi Co basin(wesetern Tibet)since 13000yrB.P. Quaternary Research,1993, 39(1):300-313.

[23] Xu Q H, Li Y C, Bunting M J, et al. The effects of trainingset selection on the relationship between pollen assemblagesand climate parameters: Implications. Palaeogeography,Palaeoclimatology, Palaeoecology, 2010, doi:10.1016/j.palaeo.2010.02.024.

[24] 龚高法, 张丕远, 吴祥定, 等. 历史时期气候变化研究方法. 北京: 科学出版社, 1983: 6-7.

[25] 赵东升, 李双成, 吴绍洪. 青藏高原的气候植被模型研究进展. 地理科学进展, 2006, 25(4): 68-78.

[26] 于学峰, 周卫健, Franzen G L, 等. 青藏高原东部全新世冬夏季风变化的高分辨率泥炭记录. 中国科学: D 辑,2006, 36(2): 182-187.

[27] 刘兴起, 沈吉, 王苏民, 等. 青海湖16 ka以来的花粉记录及其古气候古环境演化. 科学通报, 2002, 47(17):1351-1355.

[28] Gasse F, Arnold M, Fontes J C, et al. A 13000 year climaterecord from western Tibet. Nature, 1991, 353(4):742-745.

[29] Dykoski C A, Edwards R L, Cheng H, et al. A high-resolution,absolute-dated Holocene and deglacial Asian monsoonrecord from Dongge Cave, China. Earth and PlanetaryScience Letters, 2005, 233(6): 71- 86.

[30] 王富葆. 青藏高原全新世气候及环境基本特征//施雅风.中国全新世大暖期气候与环境. 北京: 海洋出版社, 1992: 197-205.

[31] 靳鹤龄, 董光荣, 苏志珠, 等. 全新世沙漠—黄土边界带空间格局的重建. 科学通报, 2001, 46(7): 538-543.

青藏高原全新世降水序列的集成重建

Synthetical Reconstruction of the Precipitation Series of the Qinghai-Tibet Plateau during the Holocene

PDF (PC)

赞

可视化

被引次数

摘要/Abstract

引用本文

使用本文

参考文献

相关文章 15

Metrics

本文评价

推荐阅读 0

[1]	张灵, 张俊, 杜良敏, 高雅琦. 长江上游降水对三峡水库蓄水关键月入库流量的影响[J]. 地理科学进展, 2020, 39(7): 1117-1125.
[2]	孙赫, 苏凤阁. 雅鲁藏布江流域多源降水产品评估及其在水文模拟中的应用[J]. 地理科学进展, 2020, 39(7): 1126-1139.
[3]	陈瑞, 杨梅学, 万国宁, 王学佳. 基于水热变化的青藏高原土壤冻融过程研究进展[J]. 地理科学进展, 2020, 39(11): 1944-1958.
[4]	王婧, 李海蓉, 杨林生. 青藏高原大骨节病流行区环境、食物及人群硒水平研究[J]. 地理科学进展, 2020, 39(10): 1677-1686.
[5]	周玉科. 青藏高原植被NDVI对气候因子响应的格兰杰效应分析[J]. 地理科学进展, 2019, 38(5): 718-730.
[6]	徐明, 石玉立, 王彬. 高分辨率青藏高原历史月降水数据重建[J]. 地理科学进展, 2018, 37(7): 923-932.
[7]	张芳芳, 郑永宏, 潘国艳, 袁帅, 孔繁希, 起永东, 王丹. 神农架地区树轮δ¹⁸O序列的气候指示意义[J]. 地理科学进展, 2018, 37(7): 946-953.
[8]	吉振明. 青藏高原黑碳气溶胶外源传输及气候效应模拟研究进展与展望[J]. 地理科学进展, 2018, 37(4): 465-475.
[9]	朱燕, 侯光良, 兰措卓玛, 高靖易, 庞龙辉. 基于GIS的青藏高原史前交通路线与分区分析[J]. 地理科学进展, 2018, 37(3): 438-449.
[10]	张国庆. 青藏高原湖泊变化遥感监测及其对气候变化的响应研究进展[J]. 地理科学进展, 2018, 37(2): 214-223.
[11]	朱艳欣, 桑燕芳. 青藏高原降水季节分配的空间变化特征[J]. 地理科学进展, 2018, 37(11): 1533-1544.
[12]	温小洁, 姚顺波, 赵敏娟. 基于降水条件的城镇化与植被覆盖协调发展研究[J]. 地理科学进展, 2018, 37(10): 1352-1361.
[13]	郭禹含, 王中根, 伍玉良. 多源再分析降水数据在拉萨河流域应用对比研究[J]. 地理科学进展, 2017, 36(8): 1033-1039.
[14]	刘翀, 朱立平, 王君波, 乔宝晋, 鞠建廷, 黄磊. 基于MODIS的青藏高原湖泊透明度遥感反演[J]. 地理科学进展, 2017, 36(5): 597-609.
[15]	王婷. 2009-2015年国际青藏高原研究文献计量分析——基于SCIE和ESI数据[J]. 地理科学进展, 2017, 36(4): 500-512.