用户名: 密码: 验证码:
Climatic classification over asia during the middle holocene climatic optimum based on PMIP models
详细信息    查看全文
  • 作者:Hyuntaik Oh ; Ho-Jeong Shin
  • 关键词:paleoclimate modeling intercomparison project (PMIP) ; paleoclimate ; global warming ; Asian continent
  • 刊名:Journal of Earth Science
  • 出版年:2016
  • 出版时间:February 2016
  • 年:2016
  • 卷:27
  • 期:1
  • 页码:123-129
  • 全文大小:1,366 KB
  • 参考文献:An, Z. S., Porter, S. C., Kutzbach, J. E., et al., 2000. Asynchronous Holocene Optimum of the East Asian Monsoon. Quaternary Science Reviews, 19(8): 743–762CrossRef
    Bond, G., Kromer, B., Beer, J., et al., 2001. Persistent Solar Influence on North Atlantic Climate during the Holocene. Science, 294(5549): 2130–2136CrossRef
    Braconnot, P., Joussaume, S., de Noblet, N., et al., 2000. Mid-Holocene and Last Glacial Maximum African Monsoon Changes as Simulated within the Paleoclimate Modelling Intercomparison Project. Global and Planetary Change, 26(1): 51–66CrossRef
    Braconnot, P., Harrison, S. P., Joussaume, S., et al., 2004. Evaluation of PMIP Coupled Ocean-Atmosphere Simulations of the Mid-Holocene. In: Battarbee, R. W., Gasse, F., Stickley, C. E., eds., Past Climate Variability through Europe and Africa. Springer, Dordrecht. 515–33CrossRef
    Braconnot, P., Otto-Bliesner, B., Harrison, S. P., et al., 2007a. Results of PMIP2 Coupled Simulations of the Mid-Holocene and Last Glacial Maximum—Part 1: Experiments and Large-Scale Features. Climate of the Past, 3(2): 261–277CrossRef
    Braconnot, P., Otto-Bliesner, B., Harrison, S. P., et al., 2007b. Results of PMIP2 Coupled Simulations of the Mid-Holocene and Last Glacial Maximum, Part 2: Feedbacks with Emphasis on the Location of the ITCZ and Mid-and High Latitudes Heat Budget. Climate of the Past, 3(2): 279–296CrossRef
    Braconnot, P., Harrison, S. P., Kageyama, M., et al., 2012. Evaluation of Climate Models Using Palaeoclimatic Data. Nature Climate Change, 2(6): 417–424CrossRef
    Chen, F. H., Yu, Z. C., Yang, M. L., et al., 2008. Holocene Moisture Evolution in Arid Central Asia and Its out-of-Phase Relationship with Asian Monsoon History. Quaternary Science Reviews, 27(3): 351–364CrossRef
    Covey, C., AchutaRao, K. M., Lambert, S. J., et al., 2000. Intercomparison of Present and Future Climates Simulated by Coupled Ocean-Atmosphere GCMs. Program for Climate Model Diagnosis and Intercomparison. Rep. 66, Program for Clim. Model Diag. and Intercomparison, Lawrence Livermore Natl. Lab., Univ. of Calif., LivermoreCrossRef
    Crowley, T. J., 2000. Causes of Climate Change over the Past 1 000 Years. Science, 289(5477): 270–277CrossRef
    Crucifix, M., Loutre, M.-F., Tulkens, P., et al., 2002. Climate Evolution during the Holocene: A Study with an Earth System Model of Intermediate Complexity. Climate Dynamics, 19(1): 43–60CrossRef
    Gotanda, K., Nakagawa, T., Tarasov, P., et al., 2002. Biome Classification from Japanese Pollen Data: Application to Modern-Day and Late Quaternary Samples. Quaternary Science Reviews, 21(4): 647–657CrossRef
    Gupta, A. K., Anderson, D. M., Overpeck, J. T., 2003. Abrupt Changes in the Asian Southwest Monsoon during the Holocene and Their Links to the North Atlantic Ocean. Nature, 421(6921): 354–357CrossRef
    Harrison, S. P., Jolly, D., Laarif, F., et al., 1998. Intercomparison of Simulated Global Vegetation Distributions in Response to 6 kyr BP Orbital Forcing. Journal of Climate, 11(11): 2721–2742CrossRef
    Harrison, S. P., Prentice, C. I., 2003. Climate and CO2 Controls on Global Vegetation Distribution at the Last Glacial Maximum: Analysis Based on Palaeovegetation Data, Biome Modelling and Palaeoclimate Simulations. Global Change Biology, 9(7): 983–1004CrossRef
    Harrison, S. P., Yu, G., Takahara, H., et al., 2001. Palaeovegetation (Communications Arising): Diversity of Temperate Plants in East Asia. Nature, 413(6852): 129–130CrossRef
    Haywood, A. M., Valdes, P. J., Sellwood, B. W., 2000. Global Scale Palaeoclimate Reconstruction of the Middle Pliocene Climate Using the UKMO GCM: Initial Results. Global and Planetary Change, 25(3): 239–256CrossRef
    He, Y. Q., Theakstone, W. H., Zhang, Z. L., et al., 2004. Asynchronous Holocene Climatic Change across China. Quaternary Research, 61(1): 52–63CrossRef
    Iorio, J. P., Guilderson, T., 2002. Holocene Climate of the Mesotropics and Comparison of Paleodata Climate Reconstruction with PMIP Simulations of Climate at 6000 14C Years Ago. American Geophysical Union, Spring Meeting 2002, Abstract #GS41A-11
    Jansen, E., Andersson, C., Moros, M., et al., 2008. The Early to Mid-Holocene Thermal Optimum in the North Atlantic. In: Battarbee, R. W., Binney, H. A., eds., Natural Climate Variability and Global Warming: A Holocene Perspective. Blackwell Publishing Ltd.. 123–137CrossRef
    Joussaume, S., Taylor, K. E., Braconnot, P. J. F. B., et al., 1999. Monsoon Changes for 6 000 Years Ago: Results of 18 Simulations from the Paleoclimate Modeling Intercomparison Project (PMIP). Geophysical Research Letters, 26(7): 859–862CrossRef
    Joussaume, S., Taylor, K. E., 2000. The Paleoclimate Modeling Intercomparison Project. World Meteorological Organization-Publications-WMO TD. 9–24
    Karl, T. R., Trenberth, K. E., 2003. Modern Global Climate Change. Science, 302(5651): 1719–1723CrossRef
    Kattenberg, A., Giorgi, F., Grassl, H., et al., 1996. Climate Models—Projections of Future Climate. In: Houghton, J. T., Meiro Filho, L. G., Callander, B. A., et al., Climate Change 1995: The Science of Climate Change. Contribution of Working Group I to the Second Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge. 285–357
    Korotky, A. M., Razjigaeva, N. G., Grebennikova, T. A., et al., 2000. Middle-and Late-Holocene Environments and Vegetation History of Kunashir Island, Kurile Islands, Northwestern Pacific. The Holocene, 10(3): 311–331CrossRef
    Kottek, M., Grieser, J., Beck, C., et al., 2006. World Map of the Köppen-Geiger Climate Classification Updated. Meteorologische Zeitschrift, 15(3): 259–263CrossRef
    Liu, Z., Otto-Bliesner, B., Kutzbach, J., et al., 2003. Coupled Climate Simulation of the Evolution of Global Monsoons in the Holocene. Journal of Climate, 16(15): 2472–2490CrossRef
    Lohmann, U., Sausen, R., Bengtsson, L., et al., 1993. The Köppen Climate Classification as a Diagnostic Tool for General Circulation Models. Climate Research, 3: 177–193CrossRef
    Lorenz, S. J., Lohmann, G., 2004. Acceleration Technique for Milankovitch Type Forcing in a Coupled Atmosphere-Ocean Circulation Model: Method and Application for the Holocene. Climate Dynamics, 23(7/8): 727–743CrossRef
    MacCracken, M. C., 2008. Prospects for Future Climate Change and the Reasons for Early Action. Journal of the Air & Waste Management Association, 58(6): 735–786CrossRef
    Masson, V., Joussaume, S., Pinot, S., et al., 1998. Impact of Parameterizations on Simulated Winter Mid-Holocene and Last Glacial Maximum Climatic Changes in the Northern Hemisphere. Journal of Geophysical Research: Atmospheres (1984–2012), 103(D8): 8935–8946CrossRef
    Mayewski, P. A., Rohling, E. E., Stager, J. C., et al., 2004. Holocene Climate Variability. Quaternary Research, 62(3): 243–255CrossRef
    Miller, G., Mangan, J., Pollard, D., et al., 2005. Sensitivity of the Australian Monsoon to Insolation and Vegetation: Implications for Human Impact on Continental Moisture Balance. Geology, 33(1): 65–68CrossRef
    Peel, M. C., Finlayson, B. L., McMahon, T. A., 2007. Updated World Map of the Köppen-Geiger Climate Classification. Hydrology and Earth System Sciences Discussions, 4(2): 439–473CrossRef
    Prell, W. L., van Campo, E., 1986. Coherent Response of Arabian Sea Upwelling and Pollen Transport to Late Quaternary Monsoonal Winds. Nature, 323(6088): 526–528CrossRef
    Prentice, I. C., Jolly, D., 2000. Mid-Holocene and Glacial-Maximum Vegetation Geography of the Northern Continents and Africa. Journal of Biogeography, 27(3): 507–519CrossRef
    Prentice, I. C., Webb, T. III, 1998. BIOME 6000: Reconstructing Global Mid-Holocene Vegetation Patterns from Palaeoecological Records. Journal of Biogeography, 25(6): 997–1005CrossRef
    Razjigaeva, N. G., Korotky, A. M., Grebennikova, T. A., et al., 2002. Holocene Climatic Changes and Environmental History of Iturup Island, Kurile Islands, Northwestern Pacific. The Holocene, 12(4): 469–480CrossRef
    Rossignol-Strick, M., 1999. The Holocene Climatic Optimum and Pollen Records of Sapropel 1 in the Eastern Mediterranean, 9 000–6 000 BP. Quaternary Science Reviews, 18(4): 515–530CrossRef
    Shi, Y. F., Kong, Z. Z., Wang, S. M., et al., 1993. Mid-Holocene Climates and Environments in China. Global and Planetary Change, 7(1): 219–233
    Shin, H.-J., Chung, I.-U., Kim, J.-W., 2004. The Annual Variation and Closure of the Water Cycle for the Asian Continent. Journal of Climate, 17(24): 4840–4855CrossRef
    Shin, S.-I., Sardeshmukh, P. D., Webb, R. S., et al., 2006. Understanding the Mid-Holocene Climate. Journal of Climate, 19(12): 2801–2817CrossRef
    Sun, D. H., Gagan, M. K., Cheng, H., et al., 2005. Seasonal and Interannual Variability of the Mid-Holocene East Asian Monsoon in Coral Δ18O Records from the South China Sea. Earth and Planetary Science Letters, 237(1): 69–84CrossRef
    Takahara, H., Sugita, S., Harrison, S. P., et al., 2000. Pollen-Based Reconstructions of Japanese Biomes at 0, 6 000 and 18 000 14C yr BP. Journal of Biogeography, 27(3): 665–683CrossRef
    Texier, D., de Noblet, N., Harrison, S. P., et al., 1997. Quantifying the Role of Biosphere-Atmosphere Feedbacks in Climate Change: Coupled Model Simulations for 6000 Years BP and Comparison with Palaeodata for Northern Eurasia and Northern Africa. Climate Dynamics, 13(12): 865–881CrossRef
    Van Geel, B., Raspopov, O. M., Renssen, H., et al., 1999. The Role of Solar Forcing upon Climate Change. Quaternary Science Reviews, 18(3): 331–338CrossRef
    Wang, Y. J., Cheng, H., Edwards, R. L., et al., 2005. The Holocene Asian Monsoon: Links to Solar Changes and North Atlantic Climate. Science, 308(5723): 854–857CrossRef
    Wanner, H., Beer, J., Buetikofer, J., et al., 2008. Mid-to Late Holocene Climate Change: An Overview. Quaternary Science Reviews, 27(19): 1791–1828CrossRef
    Wyrwoll, K.-H., Miller, G. H., 2001. Initiation of the Australian Summer Monsoon 14 000 Years Ago. Quaternary International, 83: 119–128CrossRef
    Xiao, J. L., Nakamura, T., Lu, H. Y., et al., 2002. Holocene Climate Changes over the Desert/Loess Transition of North-Central China. Earth and Planetary Science Letters, 197(1): 11–18CrossRef
    Yi, S., 2011. Holocene Vegetation Responses to East Asian Monsoonal Changes in South Korea. In: Blanco, J., Kheradmand H., eds., Climate Change—Geophysical Foundations and Ecological Effects. InTech, Rijeka. 157–178
    Yu, G., Chen, X. D., Ni, J., et al., 2000. Palaeovegetation of China: A Pollen Data-Based Synthesis for the Mid-Holocene and Last Glacial Maximum. Journal of Biogeography, 27(3): 635–664CrossRef
    Yu, G., Prentice, I. C., Harrison, S. P., et al., 1998. Pollen-Based Biome Reconstructions for China at 0 and 6 000 Years. Journal of Biogeography, 25(6): 1055–1069CrossRef
    Yuan, D. X., Cheng, H., Edwards, R. L., et al., 2004. Timing, Duration, and Transitions of the Last Interglacial Asian Monsoon. Science, 304(5670): 575–578CrossRef
    Zhao, Y., Yu, Z. C., Chen, F. H., et al., 2009. Vegetation Response to Holocene Climate Change in Monsoon-Influenced Region of China. Earth-Science Reviews, 97(1): 242–256CrossRef
    Zhou, W. J., Yu, X. F., Jull, A. J., et al., 2004. High-Resolution Evidence from Southern China of an Early Holocene Optimum and a Mid-Holocene Dry Event during the Past 18 000 Years. Quaternary Research, 62(1): 39–48CrossRef
  • 作者单位:Hyuntaik Oh (1)
    Ho-Jeong Shin (2)

    1. Center for Marine Environmental Impact Assessment, National Fisheries Research and Development Institute, Gijang-Gun, Busan, 61975, Korea
    2. Ocean Circulation and Climate Research Division, Korea Institute of Ocean Science and Technology, Sangrok-gu, Ansan-si, 15627, Korea
  • 刊物主题:Earth Sciences, general; Geotechnical Engineering & Applied Earth Sciences; Biogeosciences; Geochemistry; Geology;
  • 出版者:Springer Berlin Heidelberg
  • ISSN:1867-111X
文摘
When considering potential global warming projections, it is useful to understand the impact of each climate condition at 6 kyr before present. Asian paleoclimate was simulated by performing an integration of the multi-model ensemble with the paleoclimate modeling intercomparison project (PMIP) models. The reconstructed winter (summer) surface air temperature at 6 kyr before present was 0.85 ºC (0.21 ºC) lower (higher) than the present day over Asia, 60ºE–150ºE, 10ºN–60ºN. The seasonal variation and heating differences of land and ocean in summer at 6 kyr before present might be much larger than present day. The winter and summer precipitation of 6 kyr before present were 0.067 and 0.017 mm·day-1 larger than present day, respectively. The Group B climate, which means the dry climates based on Köppen climate classification, at 6 kyr before present decreased 17% compared to present day, but the Group D which means the continental and microthermal climates at 6 kyr before present increased over 7%. Comparison between the results from the model simulation and published paleo-proxy record agrees within the limited sparse paleo-proxy record data. Key Words paleoclimate modeling intercomparison project (PMIP) paleoclimate global warming Asian continent

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700