Abstract
The Amazon basin is a global center of hydroclimatic variability and biodiversity, but there are only eight instrumental rainfall stations with continuous records longer than 80 years in the entire basin, an area nearly the size of the coterminous US. The first long moisture-sensitive tree-ring chronology has been developed in the eastern equatorial Amazon of Brazil based on dendrochronological analysis of Cedrela cross sections cut during sustainable logging operations near the Rio Paru. The Rio Paru chronology dates from 1786 to 2016 and is significantly correlated with instrumental precipitation observations from 1939 to 2016. The strength and spatial scale of the precipitation signal vary during the instrumental period, but the Rio Paru chronology has been used to develop a preliminary reconstruction of February to November rainfall totals from 1786 to 2016. The reconstruction is related to SSTs in the Atlantic and especially the tropical Pacific, similar to the stronger pattern of association computed for the instrumental rainfall data from the eastern Amazon. The tree-ring data estimate extended drought and wet episodes in the mid- to late-nineteenth century, providing a valuable, long-term perspective on the moisture changes expected to emerge over the Amazon in the coming century due to deforestation and anthropogenic climate change.
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References
Baker JCA, Hunt SFP, Clerici SJ et al (2015) Oxygen isotopes in tree rings show good coherence between species and sites in Bolivia. Glob Planet Change 133:298–308
Becker A, Meyer-Christoffer A, Rudolf B, Schamm K, Schneider U, Ziese M (2013) A description of the global land-surface precipitation data products of the Global Precipitation Climatology Centre with sample applications including centennial (trend) analysis from 1901–present. Earth Syst Sci Data 5:71–99. https://doi.org/10.5194/essd-5-71-2013
Bräuning A, Volland-Voigt F, Burchardt I et al (2009) Climatic control of radial growth of Cedrela montana in a humid mountain rainforest in southern Ecuador. Erdkunde 63:337–345
Brienen R, Zuidema P (2005) Relating tree growth to rainfall in Bolivian rain forests: a test for six species using tree ring analysis. Oecologia 146:1–12. https://doi.org/10.1007/s00442-005-0160-y
Brienen RJW, Helle G, Pons TL, Guyot J-L, Gloor M (2012) Oxygen isotopes in tree rings are a good proxy for Amazonian precipitation and ENSO variability. Proc Nat Acad Sci 109:16957–16962. https://doi.org/10.1073/pnas.1205977109/-/DCSupplemental
Callede J, Guyot JL, Ronchail J, L’Hote Y, de Oliveira HNE (2004) Evolution du debit de l’Amazone a Obidos de 1903 a 1999/Evolution of the River Amazon’s discharge at Obidos from 1903 to 1999. Hydrol Sci J 49:85–97
Cardoso D et al (2017) Amazon plant diversity revealed by a taxonomically verified species list. Proc Nat Academy Sci. https://doi.org/10.1073/pnas.1706756114
Chagnon FJF, Bras RL (2005) Contemporary climate change in the Amazon. Geophys Res Lett 32:L13703. https://doi.org/10.1029/2005GL022722
Cook ER (1985) A Time series analysis approach to tree-ring standardization. Dissertation, The University of Arizona
Cook ER, Krusic PJ (2005) Program ARSTAN: a tree-ring standardization program based on detrending and autoregressive time series modeling, with interactive graphics. Manuscript on file, Tree-Ring Lab. Lamont Doherty Earth Observatory of Columbia University, Palisades
Cook ER, Pederson N (2011) Uncertainty, emergence, and statistics in dendrochronology. Dendroclimatology, developments in Paleoenvironmental Research. In: Hughes MK, Swetnam TW, Diaz HF (eds) Progress and prospects, vol 11. Springer, Berlin, pp 77–112
Cook ER, Meko DM, Stahle DW, Cleaveland MK (1999) Drought reconstructions for the continental United States. J Clim 12:1145–1162
Cook ER, Seager R, Heim Jr RR, Vose RS, Herweijer C, Woodhouse C (2010) Megadroughts in North America: placing IPCC projections of hydroclimatic change in a long-term palaeoclimate context. J Quat Sci 25:48–61. https://doi.org/10.1002/jqs.1303
Cook ER, Palmer JG, Ahmed M, Woodhouse CA, Fenwick P, Zafar MU, Wahab M, Khan N (2013) Five centuries of upper Indus River flow from tree rings. J Hydrol 486:365–375
Costa MH, Botta A, Cardille J (2003) Effects of large-scale change in land cover on the discharge of the Tocantins River. Amazonia J Hydrol 283:206–217
Crutzen P (1987) Role of the tropics in atmospheric chemistry. In: Dickinson RE (ed) The geophysiology of Amazonia: vegetation and climate interactions. Wiley, New York, pp 107–132
Douglass AE (1941) Crossdating in dendrochronology. J For 39:825–831
Dünisch O, Bauch J, Gasparotto L (2002) Formation of increment zones and intraannual growth dynamics in the xylem of Swietenia macrophylla, Carapa guianensis, and Cedrela odorata (Meliaceae). IAWA J 23:101–119
Fritts HC (1966) Growth rings of trees: their correlation with climate. Science 154:973–979
Gentry AH, Lopez-Parodi J (1980) Deforestation and increased flooding of the Upper Amazon. Science 210:1354–1356
Gloor M, Brienen RJW, Galbraith D, Feldpausch TR, Schöngart J, Guyot JL, Espinoza JC, Lloyd J, Phillips OL (2013) Intensification of the Amazon hydrological cycle over the last two decades. Geophys Res Lett 40:1729–1733. https://doi.org/10.1002/grl.50377
Gloor M, Barichivich J, Ziv G, Brienen R, Schöngart J, Peylin P, Barcante Ladvocat Cintra B, Feldpausch T, Phillips O, Baker J (2015) Recent Amazon climate as background for possible ongoing and future changes of Amazon humid forests. Glob Biogeochem Cycles. https://doi.org/10.1002/2014GB005080
Griffin RD, Woodhouse CA, Meko DM, Stahle DW, Faulstich HL, Carrillo C, Touchan R, Castro CL, andLeavitt SW (2013) North American monsoon precipitation reconstructed from tree rings. Geophys Res Lett. https://doi.org/10.1002/grl.50184
Harris I, Jones PD, Osborn TJ, Lister DH (2014) Updated high resolution grids of monthly climatic observations—the CRU TS3.10 dataset. Int J Climatol 34:623–642. https://doi.org/10.1002/joc.3711
Hilker T, Lyapustin AI, Tucker CJ, Hall FG, Myneni RB, Wang Y, Bi J, Mendes de Moura Y, Sellers PJ (2014) Vegetation dynamics and rainfall sensitivity of the Amazon. Proc Nat Acad Sci 111:16041–16046. https://doi.org/10.1073/pnas.1404870111
Holmes RL (1983) Computer-assisted quality control in tree-ring dating and measurement. Tree Ring Bull 44:69–78
Intergovernmental Panel on Climate Change (2013) Climate change 2013: the physical science basis. In: Stocker TF et al (eds) Contribution of working group i to the fifth assessment report of the intergovernmental panel on climate change (IPCC). Cambridge University Press, Cambridge
Ishii M, Shouji A, Sugimoto S, Matsumoto T (2005) Objective analyses of sea-surface temperature and marine meteorological variables for the 20th century using ICOADS and the Kobe collection. Int J Climatol 25:865–879. https://doi.org/10.1002/joc.1169
Kalnay E et al (1996) The NCEP/NCAR 40-year reanalysis project. BAMS 77:437–471
Khanna J, Medvigy D, Fueglistaler S, Walko R (2017) Regional dry-season climate changes due to three decades of Amazonian deforestation. Nat Clim Change 7:200–204
Lewis SL, Brando PM, Phillips OL, Van der Heijden GMF, Nepstad D (2011) The 2010 Amazon drought. Science 331:554. https://doi.org/10.1126/science.1200807
Lopez L, Villalba R (2011) Climate influences on the radial growth of Centrolobium microchaete, a valuable timber species from tropical dry forests in Bolivia. Biotropica 43:41–49. https://doi.org/10.1111/j.1744-7429.2010.00653.x
Lopez L, Villalba R (2016) Reliable estimates of radial growth for eight tropical species based on wood anatomical patterns. J Trop For Sci 28:139–152
López L, Stahle D, Villalba R, Torbenson M, Feng S, Cook E (2017) Tree-ring reconstructed rainfall over the southern Amazon Basin. Geophys Res Lett 44:7410–7418. https://doi.org/10.1002/2017GL073363
Malhi Y, Roberts JT, Betts RA (2008) Climate change and the fate of the Amazon. Philos Trans R Soc B Biol Sci 363:1727–1932. https://doi.org/10.1126/science.1146961
Marengo JA, Espinoza JC (2016) Extreme seasonal droughts and floods in Amazonia: causes, trends and impacts. Int J Climatol 36:1033–1050. https://doi.org/10.1002/joc.4420
Meko DM, Cook ER, Stahle DW, Stockton CW, Hughes MK (1993) Spatial patterns of tree-growth anomalies in the United States and southeastern Canada. J Clim 6:1773–1786
Nobre CA, Sampiao G, Borma LS, Castilla-Rubio JC, Silva JS, M Cardoso M (2016) Land-use and climate change risks in the Amazon and the need of a novel sustainable development paradigm. Proc Nat Acad Sci 113:10759–10768
Olive DJ (2007) Prediction intervals for regression models. Comput Stat Data Anal 51:3115–3122. https://doi.org/10.1016/j.csda.2006.02.006
Paredes-Villanueva K, López L, Cerrillo RMN (2016) Regional chronologies of Cedrela fissilis and Cedrela angustifolia in three forest types and their relation to climate. Trees. https://doi.org/10.1007/s00468-016-1391-8
Richey JE, Nobre C, Deser C (1989) Amazon River discharge and climate variability: 1903–1985. Science 246:101–103
Schneider U, Finger P, Meyer-Christoffer A, Rustemeier E, Ziese M, Becker A (2017) Evaluating the hydrological cycle over land using the newly-corrected precipitation climatology from the Global Precipitation Climatology Centre (GPCC). Atmosphere 8:52. https://doi.org/10.3390/atmos8030052
Schöngart J, Bräuning A, Barbosa ACMC., Lisi CS, de Oliveira JM (2017) Dendroecological studies in the neotropics: history, status and future challenges. In: Amoroso M, Daniels L, Baker P, Camarero J (eds) Dendroecology. ecological studies (analysis and synthesis), vol 231. Springer, Cham, pp 35–73
Schulman E (1956) Dendroclimatic changes in semi-arid America. University of Arizona Press, Tucson
Seber A, Lee J (2003) Linear regression analysis. Wiley, Hoboken
Stokes MA, Smiley TL (1996) An introduction to tree-ring dating. University of Arizona Press, Tucson
ter Steege H, Pitman NCA, Sabatier D, Baraloto C, Salomão RP et al (2013) Hypredominance in the Amazonian tree flora. Science 342:325–334
ter Steege H, Vaessen RW, Cardenes-Lopez D, Sabatier D, Antonelli A, Mota de Oliveira S, Pitman NCA, Jorgensem PM, Salomao RP (2016) The discovery of the Amazonian tree flora with an updated checklist of all known tree taxa. Sci Rep 6:29549. https://doi.org/10.1038/srep29549
Torralba V, Rodríguez-Fonseca B, Mohino E, Losada T (2015) The non-stationary influence of the Atlantic and Pacific Niños on North Eastern South American rainfall. Front Earth Sci 3. https://doi.org/10.3389/feart.2015.00055
van der Schrier G, Barichivich J, Briffa KR, Jones PD (2013) A scPDSI-based global data set of dry and wet spells for 1901–2009. J Geophys Res Atmos 118:4025–4048
Villalba R, Cook ER, Jacoby GC, D’Arrigo RD, Veblen TT, Jones PD (1998) Tree-ring based reconstructions of northern Patagonia precipitation since AD 1600. Holocene 8:659–674
Villalba R, Lara A, Masiokas MH, Urrutia R, Luckman BH, Marshall GJ (2012) Nat Geosci 5:793. https://doi.org/10.1038/NGEO1613
Vinod HD (2006) Maximum entropy ensembles for time series inference in economics. J Asian Econ 17:955–978. https://doi.org/10.1016/j.asieco.2006.09.001
Wagner FH et al (2014) Climate seasonality limits leaf carbon assimilation and wood productivity in tropical forests. Biogeosciences 13:2537–2562
Wang H, Fu R (2007) The influence of Amazon rainfall on the Atlantic ITCZ through convectively coupled Kelvin waves. J Clim 20:1188–1201
Wigley TML, Briffa KR, Jones PD (1984) On the average value of correlated time series, with applications in dendroclimatology and hydrometeorology. J Clim Appl Meteorol 23:201–213
Acknowledgements
This study has been funded by the U.S. National Science Foundation (Grant Number AGS-1501321) and is based on the collaboration between the Federal University at Lavras, the Brazilian National Institute of Amazonian Research (INPA) at Manaus, the Argentine Institute of Snow Research, Glaciology, and Environmental Sciences (IANIGLA) in Mendoza, and the University of Arkansas, Fayetteville. D. Granato-Souza was funded in Brazil by the Coordination for the Improvement of Higher Education Personnel (CAPES). We gratefully acknowledge the extensive logistical support and wood donations from Norte Energia (Gilberto Veronese, Miguel Lanzuolo de Paula, Daniel Angelo, Elmar Araújo, José Maria, especially, Jailton Rodriguez Bajos), LEME Energia, the Hudson logging company, and Sr. Evandro Dalmaso and Sra. Eliane Dalmaso of the CEMAL logging firm for their generous logistical support and hospitality. GPCC Precipitation data provided by the NOAA/OAR/ESRL PSD, Boulder, Colorado, USA, from their Web site at http://www.esrl.noaa.gov/psd/. COBE SST data provided by the NOAA/OAR/ESRL PSD, Boulder, Colorado, USA, from their Web site at http://www.esrl.noaa.gov/psd/. The indices of the Atlantic Meridional Mode were provided by NOAA at https://www.esrl.noaa.gov/psd/data/timeseries/monthly/AMM/. We thank two reviewers for suggestions that helped improve this article. We also acknowledge the data provided by the Climatic Research Unit, University of East Anglia, and the use of the KNMI Climate Explorer. The data developed for this article have been contributed to the International Tree-Ring Data Bank at the NOAA Paleoclimatology Program, including all tree-ring data, the instrumental four-station precipitation data, and the derived reconstruction: https://www.ncdc.noaa.gov/data-access/paleoclimatology-data.
Funding
This study was funded by U.S. National Science Foundation (Grant number AGS-1501321) to the University of Arkansas, and by the Conselho Nacional de Desenvolvimento Científico e Tecnológico (CNPq) to the Federal University of Lavras.
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Granato-Souza, D., Stahle, D.W., Barbosa, A.C. et al. Tree rings and rainfall in the equatorial Amazon. Clim Dyn 52, 1857–1869 (2019). https://doi.org/10.1007/s00382-018-4227-y
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DOI: https://doi.org/10.1007/s00382-018-4227-y