Milly, P. C., Dunne, Okay. A. & Vecchia, A. V. International sample of traits in streamflow and water availability in a altering local weather. Nature 438, 347–350 (2005).
Yao, T. et al. Latest Third Pole’s speedy warming accompanies cryospheric soften and water cycle intensification and interactions between monsoon and setting: multidisciplinary strategy with observations, modeling, and evaluation. Bull. Am. Meteorol. Soc. 100, 423–444 (2019).
Brun, F., Berthier, E., Wagnon, P., Kääb, A. & Treichler, D. A spatially resolved estimate of Excessive Mountain Asia glacier mass balances from 2000 to 2016. Nat. Geosci. 10, 668–673 (2017).
Dehecq, A. et al. Twenty-first century glacier slowdown pushed by mass loss in Excessive Mountain Asia. Nat. Geosci. 12, 22–27 (2019).
Immerzeel, W. W., Van Beek, L. P. & Bierkens, M. F. Local weather change will have an effect on the Asian water towers. Science 328, 1382–1385 (2010).
Kraaijenbrink, P. D. A., Bierkens, M. F. P., Lutz, A. F. & Immerzeel, W. W. Affect of a worldwide temperature rise of 1.5 levels Celsius on Asia’s glaciers. Nature 549, 257–260 (2017).
Bolch, T. Hydrology: Asian glaciers are a dependable water supply. Nature 545, 161–162 (2017).
Lutz, A. F., Immerzeel, W. W., Shrestha, A. B. & Bierkens, M. F. P. Constant improve in Excessive Asia’s runoff because of growing glacier soften and precipitation. Nat. Clim. Change 4, 587–592 (2014).
Chellaney, B. Water: Asia’s New Battleground (Georgetown Univ. Press, 2011).
Liang, Y., Chen, Y., Chen, F. & Zhang, H. Potential function of the regional NDVI within the growth of the Chiefdom of Lijiang throughout the Ming Dynasty as mirrored by historic paperwork and tree rings. Climate Clim. Soc. 14, 1107–1118 (2022).
Wang, T. et al. Atmospheric dynamic constraints on Tibetan Plateau freshwater below Paris local weather targets. Nat. Clim. Change 11, 219–225 (2021).
Lieberman, V. & Buckley, B. The impression of local weather on Southeast Asia, circa 950–1820: New findings. Mod. Asian Stud. 46, 1049–1096 (2012).
Buckley, B. M., Fletcher, R., Wang, S. Y. S., Zottoli, B. & Pottier, C. Monsoon extremes and society over the previous millennium on mainland Southeast Asia. Quat. Sci. Rev. 95, 1–19 (2014).
Day, M. B. et al. Paleoenvironmental historical past of the west Baray, Angkor (Cambodia). Proc. Natl Acad. Sci. USA 109, 1046–1051 (2012).
Fletcher, R., Buckley, B. M., Pottier, C. & Wang, S. Y. S. in Megadrought and Collapse: From Early Agriculture to Angkor (ed. Weiss, H.) 275–314 (2017).
Prepare dinner, E. R. et al. Asian monsoon failure and megadrought over the last millennium. Science 328, 486–489 (2010).
Buckley, B. M. et al. Local weather as a contributing issue within the demise of Angkor, Cambodia. Proc. Natl Acad. Sci. USA 107, 6748–6752 (2010).
Chen, F. et al. Ecological and societal results of Central Asian streamflow variation over the previous eight centuries. NPJ Clim. Atmos. Sci. 5, 1–8 (2022).
DeMenocal, P. B. Cultural responses to local weather change throughout the late Holocene. Science 292, 667–673 (2001).
Lieberman, V. Constitution state collapse in Southeast Asia, ca. 1250–1400, as an issue in regional and world historical past. Am. Hist. Rev. 116, 937–963 (2011).
Fox, J. & Ledgerwood, J. Dry-season flood-recession rice within the Mekong Delta: two thousand years of sustainable agriculture? Asian Perspect. 38, 37–50 (1999).
Grill, G. et al. Mapping the world’s free-flowing rivers. Nature 569, 215–221 (2019).
Gao, J., Yao, T., Masson-Delmotte, V., Steen-Larsen, H. C. & Wang, W. Collapsing glaciers threaten Asia’s water provides. Nature 565, 19–21 (2019).
Schmitt, R. J., Bizzi, S., Castelletti, A., Opperman, J. J. & Kondolf, G. M. Planning dam portfolios for low sediment trapping exhibits limits for sustainable hydropower within the Mekong. Sci. Adv. 5, eaaw2175 (2019).
Sabo, J. L. et al. Designing river flows to enhance meals safety futures within the Decrease Mekong Basin. Science 358, eaao1053 (2017).
Fendorf, S., Michael, H. A. & van Geen, A. Spatial and temporal variations of groundwater arsenic in South and Southeast Asia. Science 328, 1123–1127 (2010).
Hackney, C. R. River financial institution instability from unsustainable sand mining within the decrease Mekong River. Nat. Maintain. 3, 1–9 (2020).
Pritchard, H. D. Asia’s shrinking glaciers defend giant populations from drought stress. Nature 569, 649–654 (2019).
Veldkamp, T. I. E. et al. Water shortage hotspots journey downstream because of human interventions within the twentieth and twenty first century. Nat. Commun. 8, 1–12 (2017).
Mekonnen, M. M. & Hoekstra, A. Y. 4 billion folks going through extreme water shortage. Sci. Adv. 2, e1500323 (2016).
Qi, W., Liu, J., Xia, J. & Chen, D. Divergent sensitivity of floor water and vitality variables to precipitation product uncertainty within the Tibetan Plateau. J. Hydrol. 581, 124338 (2020).
Liu, W. et al. Investigating water price range dynamics in 18 river basins throughout the Tibetan Plateau by way of a number of datasets. Hydrol. Earth Syst. Sci. 22, 351–371 (2018).
Prepare dinner, E. R. et al. 5 centuries of Higher Indus River movement from tree rings. J. Hydrol. 486, 365–375 (2013).
Chen, F. et al. 500-12 months tree-ring reconstruction of Salween River streamflow associated to the historical past of water provide in Southeast Asia. Clim. Dyn. 53, 6595–6607 (2019).
Nguyen, H. T., Turner, S. W., Buckley, B. M. & Galelli, S. Coherent streamflow variability in monsoon Asia over the previous eight centuries-Hyperlinks to oceanic drivers. Water Resour. Res. 56, e2020WR027883 (2020).
Rao, M. P. et al. Seven centuries of reconstructed Brahmaputra River discharge exhibit underestimated excessive discharge and flood hazard frequency. Nat. Commun. 11, 1–10 (2020).
Wu, Y. et al. Reconstructed eight-century streamflow within the Tibetan Plateau reveals contrasting regional variability and powerful nonstationarity. Nat. Commun. 13, 1–13 (2022).
Otto-Bliesner, B. L. et al. Local weather variability and alter since 850 CE: an ensemble strategy with the Neighborhood Earth System Mannequin. Bull. Am. Meteorol. Soc. 97, 735–754 (2016).
Harris, I., Osborn, T. J., Jones, P. & Lister, D. Model 4 of the CRU TS month-to-month high-resolution gridded multivariate local weather dataset. Sci. Knowledge 7, 1–18 (2020).
Ghiggi, G., Humphrey, V., Seneviratne, S. I. & Gudmundsson, L. G-RUN ENSEMBLE: a multi-forcing observation-based world runoff reanalysis. Water Resour. Res. 57, e2020WR028787 (2021).
Wang, J., Yang, B. & Ljungqvist, F. C. Moisture and temperature covariability over the Southeastern Tibetan Plateau throughout the Previous 9 Centuries. J. Clim. 33, 6583–6598 (2020).
Treydte, Okay. S. et al. The 20th century was the wettest interval in northern Pakistan over the previous millennium. Nature 440, 1179–1182 (2006).
Zhang, P. et al. A check of local weather, solar, and tradition relationships from an 1810-year Chinese language cave report. Science 322, 940–942 (2008).
Thompson, L. G. et al. A high-resolution millennial report of the South Asian monsoon from Himalayan ice cores. Science 289, 1916–1919 (2000).
Vermote, E. & NOAA CDR Program. NOAA Local weather Knowledge Report (CDR) of AVHRR Normalized Distinction Vegetation Index (NDVI), Model 5. NOAA https://doi.org/10.7289/V5ZG6QH9 (2019).
Rayner, N. A. A. et al. International analyses of sea floor temperature, sea ice, and evening marine air temperature for the reason that late nineteenth century. J. Geophys. Res. Atmos. 108, D14 (2003).
Wang, J. et al. Inner and exterior forcing of multidecadal Atlantic local weather variability over the previous 1,200 years. Nat. Geosci. 10, 512–517 (2017).
Henley, B. J. et al. A tripole index for the interdecadal Pacific oscillation. Clim. Dyn. 45, 3077–3090 (2015).
MacDonald, G. M. & Case, R. A. Variations within the Pacific Decadal Oscillation over the previous millennium. Geophys. Res. Lett. 32, L08703 (2005).
Wang, J., Yang, B. & Ljungqvist, F. C. A millennial summer time temperature reconstruction for the japanese Tibetan Plateau from tree-ring width. J. Clim. 28, 5289–5304 (2015).
Yang, Okay. et al. Latest local weather adjustments over the Tibetan Plateau and their impacts on vitality and water cycle: a assessment. Glob. Planet. Change 112, 79–91 (2014).
Tan, L. et al. Rainfall variations in central Indo-Pacific over the previous 2,700 y. Proc. Natl Acad. Sci. USA 116, 17201–17206 (2019).
Turner, A. G. & Annamalai, H. Local weather change and the South Asian summer time monsoon. Nat. Clim. Change 2, 587–595 (2012).
Kraaijenbrink, P. D., Stigter, E. E., Yao, T. & Immerzeel, W. W. Local weather change decisive for Asia’s snow meltwater provide. Nat. Clim. Change 11, 591–597 (2021).
Fan, H. & He, D. Temperature and precipitation variability and its results on streamflow within the upstream areas of the Lancang-Mekong and Nu-Salween Rivers. J. Hydrometeorol. 16, 2248–2263 (2015).
Cotterell, A. A Historical past of South-East Asia (Marshall Cavendish Worldwide, 2014).
Corridor, D. G. E. Historical past of South East Asia (Macmillan Worldwide Increased Schooling, 1981).
Wolters, O. Historical past, Tradition and Area in Southeast Asian Views (Cornell Univ. Press, 1999).
Aung-Thwin, M. & Aung-Thwin, M. A Historical past of Myanmar Since Historical Instances: Traditions and Transformations (Reaktion Books, 2013).
Baran, E., Van Zalinge, N. & Bun, N. P. Floods, floodplains and fish manufacturing within the Mekong Basin: current and previous traits. In Proc. Second Asian Wetlands Symposium, 27–30 August 2001, Penang, Malaysia pp. 920–932 (Penerbit Universiti Sains Malaysia, 2001).
Gundersen, L. G. A reassessment of the decline of the Khmer Empire. Int. J. Cult. Hist. 1, 63–66 (2015).
Carter, A. Okay. et al. Temple occupation and the tempo of collapse at Angkor Wat, Cambodia. Proc. Natl Acad. Sci. USA 116, 12226–12231 (2019).
Penny, D. & Seaside, T. P. Historic socioecological transformations within the world tropics as an Anthropocene analogue. Proc. Natl Acad. Sci. USA 118, e2022211118 (2021).
Penny, D. et al. The demise of Angkor: systemic vulnerability of city infrastructure to climatic variations. Sci. Adv. 4, eaau4029 (2018).
Bibi, S. et al. Climatic and related cryospheric, biospheric, and hydrological adjustments on the Tibetan Plateau: a assessment. Int. J. Climatol. 38, 1–17 (2018).
Wang, J. et al. Tree-ring inferred annual imply temperature variations on the southeastern Tibetan Plateau over the last millennium and their relationships with the Atlantic Multidecadal Oscillation. Clim. Dyn. 43, 627–640 (2014).
Chen, F. et al. Late twentieth century speedy improve in excessive Asian seasonal snow and glacier-derived streamflow tracked by tree rings of the higher Indus River basin. Environ. Res. Lett. 16, 094055 (2021).
Meko, D. Dendroclimatic reconstruction with time various predictor subsets of tree indices. J. Clim. 10, 687–696 (1997).
Fritts, H. C. Tree Rings and Local weather (Tutorial Press, 1976).
Zhou, J. & Tung, Okay. Okay. Deducing multidecadal anthropogenic world warming traits utilizing a number of regression evaluation. J. Atmos. Sci. 70, 3–8 (2013).
Wang, J. et al. Causes of East Asian temperature multidecadal variability since 850 ce. Geophys. Res. Lett. 45, 13–485 (2018).
Mantua, N. J., Hare, S. R., Zhang, Y., Wallace, J. M. & Francis, R. C. A Pacific interdecadal local weather oscillation with impacts on salmon manufacturing. Bull. Am. Meteorol. Soc. 78, 1069–1080 (1997).
Huang, X. et al. South Asian summer time monsoon projections constrained by the interdecadal Pacific oscillation. Sci. Adv. 6, eaay6546 (2020).
Kay, J. et al. The Neighborhood Earth System Mannequin (CESM) Giant Ensemble Venture: a group useful resource for learning local weather change within the presence of inside local weather variability. Bull. Am. Meteorol. Soc. 96, 1333e1349 (2015).
Huang, W. et al. Modifications of local weather regimes over the last millennium and the twenty-first century simulated by the Neighborhood Earth System Mannequin. Quat. Sci. Rev. 180, 42–56 (2018).
Hessl, A. E. et al. Previous and future drought in Mongolia. Sci. Adv. 4, e1701832 (2018).
Dai, A., Rasmussen, R. M., Ikeda, Okay. & Liu, C. A brand new strategy to assemble consultant future forcing information for dynamic downscaling. Clim. Dyn. 55, 315–323 (2020).
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