Solar forcing of desert vegetation and drought frequency during the last 2700 years in the interior Qaidam Basin, northeastern Tibetan Plateau
Tóm tắt
Knowledge of long-term change in vegetation and climate in semi-arid/arid regions is essential for the study of current climate and development of mitigation strategies against severe drought. Here, a fossil pollen record of annually-varved core from Sugan Lake in interior Qaidam Basin was quantitatively analyzed to reconstruct changes in vegetation, floristic diversity and drought frequency. Results of biomization suggested that regional vegetation was desert vegetation with three short-term occupations of temperate steppe/xerophytic shrub during the last 2700 years. Floristic diversity generally increased/decreased with the expansion/degradation of desert vegetation. Moisture fluctuations showed three distinct stages (extremely dry between 742BC and ∼AD500, relatively wet with an increasing trend between ∼AD500 and 1200 and relatively wet with frequent fluctuations after AD1200), interrupted by 14 drought events. Spectral analysis and continuous wavelet transform of moisture variation revealed 200- and 120-year cycles. According to cross-wavelet transform analysis, major drought frequency of ∼200-year was explicitly correlated to solar activity. It’s suggested that the centennial-scale drought frequency was mainly driven by solar activity, through modulation of large-scale atmospheric circulation. Furthermore, the effect of surface temperature-evaporation and uplifting/subsiding air flow should be notable. The climatic drought in interior Qaidam Basin could be intensified under the continuous global warming.
Tài liệu tham khảo
Berglund B E, Gaillard M J, Björkman L, Persson T. 2008. Long-term changes in floristic diversity in southern Sweden: Palynological richness, vegetation dynamics and land-use. Veg Hist Archaeobot, 17: 573–583
Birks H J B, Felde V A, Bjune A E, Grytnes J A, Seppä H, Giesecke T. 2016. Does pollen-assemblage richness reflect floristic richness? A review of recent developments and future challenges. Rev Palaeobot Palynol, 228: 1–25
Birks H J B, Line J M. 1992. The use of rarefaction analysis for estimating palynological richness from Quaternary pollen-analytical data. Holocene, 2: 1–10
Bond G, Kromer B, Beer J, Muscheler R, Evans M N, Showers W, Hoffmann S, Lotti-Bond R, Hajdas I, Bonani G. 2001. Persistent solar influence on North Atlantic climate during the Holocene. Science, 294: 2130–2136
Chen J H, Chen F H, Feng S, Huang W, Liu J B, Zhou A F. 2015. Hydroclimatic changes in China and surroundings during the Medieval Climate Anomaly and Little Ice Age: Spatial patterns and possible mechanisms. Quat Sci Rev, 107: 98–111
Chen J H, Chen F H, Zhang E L, Brooks S J, Zhou A F, Zhang J W. 2009. A 1000-year chironomid-based salinity reconstruction from varved sediments of Sugan Lake, Qaidam Basin, arid Northwest China, and its palaeoclimatic significance. Chin Sci Bull, 54: 3749–3759
Chen J H, Rao Z G, Liu J B, Huang W, Feng S, Dong G H, Hu Y, Xu Q H, Chen F H. 2016. On the timing of the East Asian summer monsoon maximum during the Holocene—Does the speleothem oxygen isotope record reflect monsoon rainfall variability? Sci China Earth Sci, 59: 2328–2338
Chen Y, Ni J, Herzschuh U. 2010. Quantifying modern biomes based on surface pollen data in China. Glob Planet Change, 74: 114–131
Colwell R K. 2013. EstimateS: Statistical estimation of species richness and shared species from samples. Version 9. User’s Guide and application. http://purl.oclc.org/estimates
Cook E R, Woodhouse C A, Eakin C M, Meko D M, Stahle D W. 2004. Long-term aridity changes in the western United States. Science, 306: 1015–1018
Cour P, Zheng Z, Duzer D, Calleja M, Yao Z. 1999. Vegetational and climatic significance of modern pollen rain in northwestern Tibet. Rev Palaeobot Palynol, 104: 183–204
Ding Y, Wang Z Y, Sun Y. 2008. Inter-decadal variation of the summer precipitation in East China and its association with decreasing Asian summer monsoon. Part I: Observed evidences. Int J Climatol, 28: 1139–1161
Dykoski C A, Edwards R L, Cheng H, Yuan D X, Cai Y J, Zhang M L, Lin Y S, Qing J M, An Z S, Revenaugh J. 2005. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge Cave, China. Earth Planet Sci Lett, 233: 71–86
El-Moslimany A P. 1990. Ecological significance of common nonarboreal pollen: Examples from drylands of the Middle East. Rev Palaeobot Palynol, 64: 343–350
Felde VA, Peglar S M, Bjune A E, Grytnes J A, Birks H J B. 2016. Modern pollen-plant richness and diversity relationships exist along a vegetational gradient in southern Norway. Holocene, 26: 163–175
Fleitmann D, Burns S J, Mudelsee M, Neff U, Kramers J, Mangini A, Matter A. 2003. Holocene forcing of the Indian monsoon recorded in a stalagmite from southern Oman. Science, 300: 1737–1739
Gasse F, Arnold M, Fontes J C, Fort M, Gibert E, Huc A, Li B Y, Li Y F, Liu Q, Melieres F, Van C E V, Wang F B, Zhang Q S. 1991. A 13000-year climate record from western Tibet. Nature, 353: 742–745
Gray L J, Beer J, Geller M, Haigh J D, Lockwood M, Matthes K, Cubasch U, Fleitmann D, Harrison G, Hood L, Luterbacher J, Meehl G A, Shindell D, van Geel B, White W. 2010. Solar influences on climate. Rev Geophys, 48: RG4001
Grinsted A, Moore J C, Jevrejeva S. 2004. Application of the cross wavelet transform and wavelet coherence to geophysical time series. Nonlin Process Geophys, 11: 561–566
Guiot J, Goeury C. 1996. PPPBase, a software for statistical analysis of paleoecological and paleoclimatological data. Dendrochronologia, 14: 295–300
Herzschuh U. 2007. Reliability of pollen ratios for environmental reconstructions on the Tibetan Plateau. J Biogeogr, 34: 1265–1273
Hou X. 2001. Vegetation Atlas of China (in Chinese). Beijing: Science Press
Huang C, Zeng T, Ye F, Wei G J. 2019. Solar-forcing-induced spatial synchronisation of the East Asian summer monsoon on centennial timescales. Palaeogeogr Palaeoclimatol Palaeoecol, 514: 536–549
Jacques JMS, Cumming B F, Smol J P. 2008. A 900-year pollen-inferred temperature and effective moisture record from varved Lake Mina, west-central Minnesota, USA. Quat Sci Rev, 27: 781–796
Kiem A S, Johnson F, Westra S, van Dijk A, Evans J P, O’Donnell A, Rouillard A, Barr C, Tyler J, Thyer M, Jakob D, Woldemeskel F, Sivakumar B, Mehrotra R. 2016. Natural hazards in Australia: Droughts. Clim Change, 139: 37–54
Li Q, Lu H Y, Zhu L P, Wu N Q, Wang J B, Lu X M. 2011. Pollen-inferred climate changes and vertical shifts of alpine vegetation belts on the northern slope of the Nyainqentanglha mountains (central Tibetan Plateau) since 8.4 kyr BP. Holocene, 21: 939–950
Li Y C, Xu Q H, Zhao Y K, Yang X L, Xiao J L, Chen H, Lu X M. 2005. Pollen indication to source plants in the eastern desert of China. Chin Sci Bull, 50: 1632–1641
Liu J B, Chen S Q, Chen J H, Zhang Z P, Chen F H. 2017. Chinese cave δ18O records do not represent northern East Asian summer monsoon rainfall. Proc Natl Acad Sci USA, 114: E2987–E2988
Liu Z Y, Wen X Y, Brady E C, Otto-Bliesner B, Yu G, Lu H Y, Cheng H, Wang Y J, Zheng W P, Ding Y H, Edwards R L, Cheng J, Liu W, Yang H. 2014. Chinese cave records and the East Asia summer monsoon. Quat Sci Rev, 83: 115–128
Lv L, Zhang Q B. 2013. Tree-ring based summer minimum temperature reconstruction for the southern edge of the Qinghai-Tibetan Plateau, China. Clim Res, 56: 91–101
Ma Q F, Zhu L P, Wang J B, Ju J T, Lü X M, Wang Y, Guo Y, Yang R M, Kasper T, Haberzettl T, Tang L Y. 2017. Artemisia/Chenopodiaceae ratio from surface lake sediments on the central and western Tibetan Plateau and its application. Palaeogeogr Palaeoclimatol Palaeoecol, 479: 138–145
Meehl G A, Arblaster J M, Matthes K, Sassi F, van Loon H. 2009. Amplifying the Pacific climate system response to a small 11-year solar cycle forcing. Science, 325: 1114–1118
Overpeck J, Anderson D, Trumbore S, Prell W. 1996. The southwest Indian Monsoon over the last 18000 years. Clim Dyn, 12: 213–225
PAGES 2k Consortium. 2019. Consistent multidecadal variability in global temperature reconstructions and simulations over the Common Era. Nat Geosci, 12: 643–649
Prentice C, Guiot J, Huntley B, Jolly D, Cheddadi R. 1996. Reconstructing biomes from palaeoecological data: A general method and its application to European pollen data at 0 and 6 ka. Clim Dyn, 12: 185–194
Rojas O, Vrieling A, Rembold F. 2011. Assessing drought probability for agricultural areas in Africa with coarse resolution remote sensing imagery. Remote Sens Environ, 115: 343–352
Schulz M, Mudelsee M. 2002. REDFIT: Estimating red-noise spectra directly from unevenly spaced paleoclimatic time series. Comput Geosci, 28: 421–426
Shao X M, Huang L, Liu H B, Liang E Y, Fang X Q, Wang L L. 2005. Reconstruction of precipitation variation from tree rings in recent 1000 years in Delingha, Qinghai. Sci China Ser D-Earth Sci, 48: 939–949
Sheffield J, Wood E F, Roderick M L. 2012. Little change in global drought over the past 60 years. Nature, 491: 435–438
Shin S I, Sardeshmukh P D, Webb R S. 2010. Optimal tropical sea surface temperature forcing of North American drought. J Clim, 23: 3907–3917
Shindell D T, Schmidt G A, Miller R L, Rind D. 2001. Northern Hemisphere winter climate response to greenhouse gas, ozone, solar, and volcanic forcing. J Geophys Res, 106: 7193–7210
Shindell D, Rind D, Balachandran N, Lean J, Lonergan P. 1999. Solar cycle variability, ozone, and climate. Science, 284: 305–308
Steinhilber F, Abreu J A, Beer J, Brunner I, Christl M, Fischer H, Heikkilä U, Kubik P W, Mann M, McCracken K G, Miller H, Miyahara H, Oerter H, Wilhelms F. 2012. 9400 years of cosmic radiation and solar activity from ice cores and tree rings. Proc Natl Acad Sci USA, 109: 5967–5971
Tan M. 2014. Circulation effect: Response of precipitation δ18O to the ENSO cycle in monsoon regions of China. Clim Dyn, 42: 1067–1077
Tian L, Masson-Delmotte V, Stievenard M, Yao T, Jouzel J. 2001. Tibetan Plateau summer monsoon northward extent revealed by measurements of water stable isotopes. J Geophys Res, 106: 28081–28088
Torrence C, Compo G P. 1998. A practical guide to wavelet analysis. Bull Amer Meteorol Soc, 79: 61–78
Usoskin I G, Hulot G, Gallet Y, Roth R, Licht A, Joos F, Kovaltsov G A, Thébault E, Khokhlov A. 2014. Evidence for distinct modes of solar activity. Astron Astrophys, 562: L10
Van Campo E, Gasse F. 1993. Pollen- and Diatom-Inferred Climatic and Hydrological Changes in Sumxi Co Basin (Western Tibet) since 13000 yr B.P. Quat Res, 39: 300–313
Van Campo E, Cour P, Sixuan H. 1996. Holocene environmental changes in Bangong Co basin (Western Tibet). Part 2: The pollen record. Palaeogeogr Palaeoclimatol Palaeoecol, 120: 49–63
Wang K C, Dickinson R E. 2013. Contribution of solar radiation to decadal temperature variability over land. Proc Natl Acad Sci USA, 110: 14877–14882
Wang S Z, Chen G C, Bai Y P, Zhou G Y, Sun Q. 2005. Interrelation between plant species diversity and soil environmental factors in Bird Island of Qinghai Lake (in Chinese). Chin J Appl Ecol, 16: 186–188
Wang Y J, Cheng H, Edwards R L, He Y Q, Kong X G, An Z S, Wu J Y, Kelly M J, Dykoski C A, Li X D. 2005. The Holocene Asian monsoon: Links to solar changes and North Atlantic climate. Science, 308: 854–857
Westman W E. 1981. Diversity relations and succession in Californian coastal sage scrub. Ecology, 62: 170–184
White W B, Lean J, Cayan D R, Dettinger M D. 1997. Response of global upper ocean temperature to changing solar irradiance. J Geophys Res, 102: 3255–3266
Wu F L, Fang X M, Herrmann M, Mosbrugger V, Miao Y F. 2011. Extended drought in the interior of Central Asia since the Pliocene reconstructed from sporopollen records. Glob Planet Change, 76: 16–21
Wu J L, Yu Z C, Zeng H A, Wang N L. 2009. Possible solar forcing of 400-year wet-dry climate cycles in northwestern China. Clim Change, 96: 473–482
Xu D K, Lu H Y, Chu G Q, Liu L, Shen C M, Li F J, Wang C, Wu N Q. 2019. Synchronous 500-year oscillations of monsoon climate and human activity in Northeast Asia. Nat Commun, 10: 4105
Yan S. 1991. The characteristics of Quaternary spore-pollen assemblage and the vegetation succession in Xinjiang (in Chinese). Arid Land Geogr, 14: 1–9
Yang B, Qin C, Wang J L, He M H, Melvin T M, Osborn T J, Briffa K R. 2014. A 3500-year tree-ring record of annual precipitation on the northeastern Tibetan Plateau. Proc Natl Acad Sci USA, 111: 2903–2908
Yu G, Tang L Y, Yang X D, Ke X K, Harrison S P. 2001. Modern pollen samples from alpine vegetation on the Tibetan Plateau. Glob Ecol Biogeogr, 10: 503–519
Yu Z C, Ito E. 1999. Possible solar forcing of century-scale drought frequency in the northern Great Plains. Geology, 27: 263–266
Zhang K, Zhao Y, Yu Z C, Zhou A F. 2010. A 2700-year high resolution pollen record of climate change from varved Sugan Lake in the Qaidam Basin, northeastern Tibetan Plateau. Palaeogeogr Palaeoclimatol Palaeoecol, 297: 290–298
Zhao Y, Herzschuh U. 2009. Modern pollen representation of source vegetation in the Qaidam Basin and surrounding mountains, north-eastern Tibetan Plateau. Veg Hist Archaeobot, 18: 245–260
Zhao Y, Liu H Y, Li F R, Huang X Z, Sun J H, Zhao W W, Herzschuh U, Tang Y. 2012. Application and limitations of the Artemisia/Chenopodiaceae pollen ratio in arid and semi-arid China. Holocene, 22: 1385–1392
Zhao Y, Yu Z C, Chen F H, Liu X J, Ito E. 2008. Sensitive response of desert vegetation to moisture change based on a near-annual resolution pollen record from Gahai Lake in the Qaidam Basin, northwest China. Glob Planet Change, 62: 107–114
Zhao Y, Yu Z C, Liu X J, Zhao C, Chen F H, Zhang K. 2010. Late Holocene vegetation and climate oscillations in the Qaidam Basin of the north-eastern Tibetan Plateau. Quat Res, 73: 59–69
Zhou A F, Chen F H, Qiang M R, Yang M L, Zhang J W. 2007. The discovery of annually laminated sediments (varves) from shallow Sugan Lake in inland arid China and their paleoclimatic significance. Sci China Ser D-Earth Sci, 50: 1218–1224