Abstract
It has been well known that the uplift of the Tibetan Plateau (TP) can significantly enhance the Asian monsoon. Here, by comparing the sensitivity experiments with and without the TP, we find that the TP uplift can also increase the precipitation of the North American Summer Monsoon (NASM), with atmosphere teleconnection accounting for 6% and oceanic dynamical process accounting for another 6%. Physically, the TP uplift generates a stationary Rossby wave train traveling from the Asian continent to the North Atlantic region, resulting in an high-pressure anomaly over the tropical-subtropical North Atlantic. This high pressure system enhances the low-level easterly winds, forcing an enhanced upward motion over the North American monsoon (NAM) region and then an increase in summer precipitation there. In addition, the TP uplift enhances the Atlantic meridional overturning circulation, which reduces the meridional temperature gradient and leads to a northward shift of Hadley Cell over eastern Pacific-Atlantic section. The latter shifts the convection center northward to 10°N and further increases the NASM precipitation. The enhanced NASM precipitation can also be understood by the northward shift of Intertropical Convergence Zone. Our study implies that the changes of NAM climate can be affected by not only local process but also remote forcing, including those from Asian highland region.
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22 July 2021
A Correction to this paper has been published: https://doi.org/10.1007/s00382-021-05888-5
References
Adam O, Bischoff T, Schneider T (2016a) Seasonal and interannual variations of the energy flux equator and ITCZ Part I: Zonally averaged ITCZ position. J Clim 29(9):3219–3230
Adam O, Bischoff T, Schneider T (2016b) Seasonal and interannual variations of the energy flux equator and ITCZ. Part II: Zonally varying shifts of the ITCZ. J Clim 29(20):7281–7293
Adams D, Comrie A (1997) The north American monsoon. Bull Am Meteor Soc 78(10):2197–2214
An Z, Kutzbach J, Prell W et al (2001) Evolution of Asian monsoons and phased uplift of the Himalaya-Tibetan plateau since Late Miocene times. Nature 411(6833):62–66
Boos WR, Korty RL (2016) Regional energy budget control of the intertropical convergence zone and application to mid-Holocene rainfall. Nat Geosci 9(12):892–897
Boos WR, Kuang Z (2010) Dominant control of the South Asian monsoon by orographic insulation versus plateau heating. Nature 463(7278):218–222
Bush ABG, Philander SGH (1999) The climate of the Last Glacial maximum: results from a coupled atmosphere-ocean general circulation model. J Geophys Res Atmos 104(D20):24509–24525
Castro CL, McKee TB Sr, Pielke RA (2001) The relationship of the North American monsoon to tropical and North Pacific sea surface temperatures as revealed by observational analyses. J Clim 14(24):4449–4473
Cerling TE, Harris JM, Ambrose SH et al (1997) Dietary and environmental reconstruction with stable isotope analyses of herbivore tooth enamel from the Miocene locality of Fort Ternan, Kenya. J Hum Evolut 33(6):635–650
Chang P, Ji L, Li H (1997) A decadal climate variation in the tropical Atlantic Ocean from thermodynamic air-sea interactions. Nature 1385(6616):516–518
Chen J, Bordoni S (2014) Orographic effects of the Tibetan Plateau on the East Asian summer monsoon: an energetic perspective. J Clim 27(8):3052–3072
Chen S, Wei K, Chen W et al (2014) Regional changes in the annual mean Hadley circulation in recent decades. J Geophys Res: Atmos 119(13):7815–7832
Cheng J, Hu S, Gao C et al (2020) On the discrepancies in the changes in the annual mean Hadley circulation among different regions and between CMIP5 models and reanalyses. Theoret Appl Climatol 141(3):1475–1491
Chiang J, Vimont D (2004) Analogous Pacific and Atlantic meridional modes of tropical atmosphere–ocean variability. J Clim 17(21):4143–4158
Chiang J, Kushnir Y, Giannini A (2002) Deconstructing Atlantic Intertropical Convergence Zone variability: Influence of the local cross‐equatorial sea surface temperature gradient and remote forcing from the eastern equatorial Pacific. Journal of Geophysical Research: Atmospheres, 107(D1): ACL 3–1-ACL 3–19.
Chou C, Neelin JD, Chen CA, Tu JY (2009) Evaluating the ‘“rich-get-richer”’ mechanism in tropical precipitation change under global warming. J Clim 22:1982–2005
Cook KH (2003) Role of continents in driving the Hadley cells. J Atmos Sci 60(7):957–976
Cook BI, Seager R (2013) The response of the North American Monsoon to increased greenhouse gas forcing. Journal of Geophysical Research: Atmospheres 118(4):1690–1699
D’Agostino R, Lionello P, Adam O et al (2017) Factors controlling Hadley circulation changes from the Last Glacial Maximum to the end of the 21st century. Geophys Res Lett 44(16):8585–8591
Dai A, Wigley T (2000) Global patterns of ENSO-induced precipitation. Geophys Res Lett 27(9):1283–1286
de Jesús Hernández-Hernández M, Cruz JA, Castañeda-Posadas C (2020) Paleoclimatic and Vegetation Reconstruction of the Miocene Southern Mexico using Fossil Flowers. J S Am Earth Sci 104:102827
Duan A, Wu G (2006) Change of cloud amount and the climate warming on the Tibetan Plateau. Geophys Res Lett 33(22)
Duan AM, Xiao ZX (2015) Does the Climate Warming Hiatus Exist Over the Tibetan Plateau? Sci Rep 5:13711
Duan A, Wu G, Liu Y et al (2012) Weather and climate effects of the Tibetan Plateau. Adv Atmos Sci 29(5):978–992
Fallah B, Cubasch U, Prömmel K et al (2016) A numerical model study on the behaviour of Asian summer monsoon and AMOC due to orographic forcing of Tibetan Plateau. Clim Dyn 47(5):1485–1495
Harrison TM, Copeland P, Kidd WSF, Yin A (1992) Raising Tibet. Science 255:1663–1670
Higgins RW, Yao Y, Wang XL (1997) Influence of the North American monsoon system on the US summer precipitation regime. J Clim 10(10):2600–2622
Hoskins BJ, Karoly DJ (1981) The steady linear response of a spherical atmosphere to thermal and orographic forcing. J Atmos Sci 38:1179–1196
Hu Q, Jiang DB, Fan GZ (2015) Climate change projection on the Tibetan Plateau: Results of CMIP5 models [in Chinese]. Chin J Atmos Sci 39:260–270
Hu S, Cheng J, Chou J (2017) Novel three-pattern decomposition of global atmospheric circulation: generalization of traditional two-dimensional decomposition. Clim Dyn 49(9):3573–3586
Hu S, Chou J, Cheng J (2018) Three-pattern decomposition of global atmospheric circulation: part I—decomposition model and theorems. Clim Dyn 50(7):2355–2368
Huber M, Goldner A (2012) Eocene monsoons. J Asian Earth Sci 44:3–23
Iqbal MJ, Rehman SU, Hameed S et al (2019) Changes in Hadley circulation: the Azores high and winter precipitation over tropical northeast Africa. Theor Appl Climatol 137(3):2941–2948
Jiang D, Ding Z, Drange H et al (2008) Sensitivity of East Asian climate to the progressive uplift and expansion of the Tibetan Plateau under the mid-Pliocene boundary conditions. Adv Atmos Sci 25(5):709–722
Julian PR, Chervin RM (1978) A study of the Southern Oscillation and Walker Circulation phenomenon. Mon Weather Rev 106:1433–1451
Kroon D, Steens T, Troelstra SR (1991) Onset of the monsoonal related upwelling in the western Arabian Sea as revealed by planktonic foraminifera. In: Prell WL et al (eds) Proceedings of the Ocean Drilling Program, Scientific results, Volume 117: College Station, Texas, Ocean Drilling Program, pp 257–263
Kushnir Y, Seager R, Ting M, Naik N, Nakamura J (2010) Mechanisms of tropical Atlantic SST influence on North American precipitation variability. J Clim 23:5610–5628
Lintner BR, Boos WR (2019) Using atmospheric energy transport to quantitatively constrain South Pacific convergence zone shifts during ENSO. J Clim 32(6):1839–1855
Liu X, Yin ZY (2002) Sensitivity of East Asian monsoon climate to the uplift of the Tibetan Plateau. Palaeogeogr Palaeoclimatol Palaeoecol 183(3–4):223–245
Liu B, Zhou T (2017) Atmospheric footprint of the recent warming slowdown. Sci Rep 7(1):1–7
Liu F, Chai J, Wang B et al (2016) Global monsoon precipitation responses to large volcanic eruptions. Sci Rep 6(1):1–11
Lu M, Yang S, Li Z et al (2018) Possible effect of the Tibetan Plateau on the “upstream” climate over west Asia, North Africa, south Europe and the North Atlantic. Clim Dyn 51(4):1485–1498
Mamalakis A, Randerson JT, Yu JY et al (2021) Zonally contrasting shifts of the tropical rain belt in response to climate change. Nat Clim Chang 1–9
Molnar P, Boos W, Battisti D (2010) Orographic controls on climate and paleoclimate of Asia: thermal and mechanical roles for the Tibetan Plateau. Annu Rev Earth Planet Sci 38(1):77–102
Nan SL, Zhao P, Yang S (2009) Springtime tropospheric temperature over the Tibetan Plateau and evolution of the tropical Pacific SST. J Geophys Res 114:D10104
Park HS, Chiang JC, Bordoni S (2012) The mechanical impact of the Tibetan Plateau on the seasonal evolution of the South Asian monsoon. J Clim 25(7):2394–2407
Parsons LA, Yin J, Overpeck JT et al (2014) Influence of the Atlantic Meridional Overturning Circulation on the monsoon rainfall and carbon balance of the American tropics. Geophys Res Lett 41(1):146–151
Pascale S, Bordoni S, Kapnick SB, Vecchi GA et al (2016) The impact of horizontal resolution on North American Monsoon Gulf of California moisture surges in a suite of coupled global climate models. J Clim 29(21):7911–7936
Pascale S, Boos WR, Bordoni S et al (2017) Weakening of the North American monsoon with global warming. Nat Clim Chang 7(11):806–812
Pascale S, Carvalho LMV, Adams DK et al (2019) Current and future variations of the monsoons of the Americas in a warming climate. Curr Clim Chang Rep 5(3):125–144
Prell WL, Kutzbach JE (1992) Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution. Nature 360(6405):647–652
Qiao S, Zou M, Tang S et al (2020) The enhancement of the impact of the wintertime North Atlantic Oscillation on the subsequent sea surface temperature over the tropical Atlantic since the middle 1990s. J Clim 33(22):9653–9672
Quade J, Cerling TE, Bowman JR (1989) Development of Asian monsoon revealed by marked ecological shift during the latest Miocene in northern Pakistan. Nature 342(6246):163–166
Rossby CG (1939) Relation between variations in the intensity of the zonal circulation of the atmosphere and the displacements of the semi-permanent centers of action. J Mar Res 2:38–55
Su B, Jiang D, Zhang R et al (2018) Difference between the North Atlantic and Pacific meridional overturning circulation in response to the uplift of the Tibetan Plateau. Clim past 14(6):751–762
Tang H, Micheels A, Eronen JT et al (2013) Asynchronous responses of East Asian and Indian summer monsoons to mountain uplift shown by regional climate modelling experiments. Clim Dyn 40(5):1531–1549
Trenberth KE, Solomon A (1994) The global heat balance: Heat transports in the atmosphere and ocean. Clim Dyn 10(3):107–134
Varuolo-Clarke AM, Reed KA, Medeiros B (2019) Characterizing the North American monsoon in the community atmosphere model: sensitivity to resolution and topography. J Clim 32(23):8355–8372
Wang B, Ding Q (2008) Global monsoon: dominant mode of annual variation in the tropics. Dyn Atmos Oceans 44(3–4):165–183
Wang B, Bao Q, Hoskins B et al (2008) Tibetan Plateau warming and precipitation changes in East Asia. Geophys Res Lett 35(14)
Wang B, Liu J, Kim HJ et al (2012) Recent change of the global monsoon precipitation (1979–2008). Clim Dyn 39(5):1123–1135
Wang C, Zhang L, Lee SK, Wu L, Mechoso CR (2014) A global perspective on CMIP5 climate model biases. Nat Clim Chang 4:201–205
Wang Z, Yang S, Duan A et al (2019) Tibetan Plateau heating as a driver of monsoon rainfall variability in Pakistan. Clim Dyn 52(9):6121–6130
Wang B, Biasutti M, Byrne MP et al (2021) Monsoons climate change assessment. Bull Am Meteorol Soc 102(1):E1–E19
Webster PJ, Magana VO et al (1998) Monsoons: processes, predictability, and the prospects for prediction. J Geophys Res 103:14451–14510
Wen Q, Yang H (2020) Investigating the role of the Tibetan Plateau in the formation of Pacific meridional overturning circulation. J Clim 33(9):3603–3617
Wen Q, Yao J, Döös K et al (2018) Decoding hosing and heating effects on global temperature and meridional circulations in a warming climate. J Clim 31(23):9605–9623
Wen Q, Döös K, Lu Z et al (2020) Investigating the role of the Tibetan Plateau in ENSO Variability. J Clim 33(11):4835–4852
Wu G, Liu Y, Dong B et al (2012) Revisiting Asian monsoon formation and change associated with Tibetan Plateau forcing: I. Formation. Clim Dyn 39(5):1169–1181
Xie SP, Deser C, Vecchi GA et al (2010) Global warming pattern formation: sea surface temperature and rainfall. J Clim 23(4):966–986
Yang H, Wen Q (2020) Investigating the role of the Tibetan Plateau in the formation of Atlantic meridional overturning circulation. J Clim 33(9):3585–3601
Yang H, Li Q, Wang K et al (2015) Decomposing the meridional heat transport in the climate system. Clim Dyn 44(9–10):2751–2768
Yang H, Wen Q, Yao J et al (2017) Bjerknes compensation in meridional heat transport under freshwater forcing and the role of climate feedback. J Clim 30(14):5167–5185
Yang H, Shen X, Yao J et al (2020) Portraying the impact of the Tibetan Plateau on global climate. J Clim 33(9):3565–3583
Zhang KX, Wang GC, Ji JL et al (2010) Paleogene-Neogene stratigraphic realm and sedimentary sequence of the Qinghai-Tibet Plateau and their response to uplift of the plateau. Sci China Earth Sci 53(9):1271–1294
Zhang RH, Su FG, Jiang ZH, Gao XJ, Guo DL, Ni J, You QL, Lan C, Zhou BT (2015) An overview of projected climate and environmental changes across the Tibetan Plateau in the 21st century [in Chinese]. Chin Sci Bull 60:3036–3047
Zhang W, Zhou T, Zhang L (2017) Wetting and greening Tibetan Plateau in early summer in recent decades. J Geophys Res 122:5808–5822
Zhao P, Zhu Y, Zhang R (2007) An Asian-Pacific teleconnection in summer tropospheric temperature and associated Asian climate variability. Climate Dyn 29:293–303
Zhao P, Yang S, Wu R, Wen Z, Chen J, Wang H (2012) Asian origin of interannual variations of summer climate over the extratropical North Atlantic Ocean. J Clim 25:6594–6609
Acknowledgements
This work is supported by the NSF of China (Nos. 91737204, 41725021, 41376007, 41630527, 4201101394, 42005012, 41971108, and 91437218), the Fundamental Research Funds for the Central Universities (Nos. B210201009), and the Natural Science Foundation of Jiangsu Province (Nos. BK20201058). The experiments were performed on the supercomputers at the Chinese National Supercomputer Centre in Tianjin (Tian-He No. 1). We thank three anonymous reviewers for their efforts to substantially improve this article.
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Wen, Q., Han, Z., Yang, H. et al. Influence of Tibetan Plateau on the North American summer monsoon precipitation. Clim Dyn 57, 3093–3110 (2021). https://doi.org/10.1007/s00382-021-05857-y
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DOI: https://doi.org/10.1007/s00382-021-05857-y