Projecting Extreme Changes in Summer Rainfall in South America by the Middle of the 21st Century

Abstract

Extreme rainfall events can be considered a natural manifestation of the environment in which they are embedded and foreknowledge about their future behavior is very important, especially for decision makers. In this context, we aimed to explore the future behavior of extreme rainfall intensity through numerical simulations with the ETA model. The model was forced with a scenario of high greenhouse gas emissions for the middle of the 21st Century as described for A1B emission scenario. We detailed the main changes in accumulated rainfall produced by heavy events, very heavy events and rare events over a broad area of South America with a focus on the tropical sector. The methodology applied here is capable of separating extreme events and establishing the quantity of rainfall yielded by them. We have found that in the near future (2041-2050) rare events will tend to increase over the Amazon basin, followed by reductions in heavy and very heavy events. Conversely, heavy, very heavy and rare events are expected to decline over north-east Brazil. Furthermore, increases were found for heavy, very heavy and rare events over southern Brazil.

Share and Cite:

M. Fonseca, P. , P. Veiga, J. , S. Correia, F. , Brito, A. , Queiroz, M. , Lyra, A. and Chou, S. (2014) Projecting Extreme Changes in Summer Rainfall in South America by the Middle of the 21st Century. Atmospheric and Climate Sciences, 4, 743-756. doi: 10.4236/acs.2014.44067.

Conflicts of Interest

The authors declare no conflicts of interest.

References

[1] Allen, M.R. and Ingram, W.J. (2002) Constraints on Future Changes in Climate and the Hydrologic Cycle. Nature, 419, 224-232. http://dx.doi.org/10.1038/nature01092
[2] Trenberth, K.E., Dai, A., Rasmussen, R.M. and Parsons, D.B. (2003) The Changing Character of Precipitation. Bulletin of the American Meteorological Society, 84, 1205-1217.
http://dx.doi.org/10.1175/BAMS-84-9-1205
[3] Hennessy, K.J., Gregory, J.M. and Mitchell, J.F.B. (1997) Changes in Daily Precipitation under Enhanced Greenhouse Conditions. Climate Dynamics, 13, 667-680.
http://dx.doi.org/10.1007/s003820050189
[4] Gordon, H.B., Whetton, P.H., Pittock, A.B., Fowler, A.M. and Haylock, M.R. (1992) Simulated Changes in Daily Rainfall Intensity Due to the Enhanced Greenhouse Effect: Implications for Extreme Rainfall Events. Climate Dynamics, 8, 83-102. http://dx.doi.org/10.1007/BF00209165
[5] Meehl, A.G., et al. (2000) Trends in Extreme Weather and Climate Events: Issues Related to Modeling Extremes in Projections of Future Climate Change. Bulletin of the American Meteorological Society, 81, 427-436. http://dx.doi.org/10.1175/1520-0477(2000)081<0427:TIEWAC>2.3.CO;2
[6] Semenov, V.A. and Bengtsson, L. (2002) Secular Trends in Daily Precipitation Characteristics: Greenhouse Gas Simulation with a Coupled AOGCM. Climate Dynamic, 19, 123-140.
http://dx.doi.org/10.1007/s00382-001-0218-4
[7] Allan, R.P. and Soden, B.J. (2008) Atmospheric Warming and the Amplification of Precipitation Extremes. Sciences, 321, 1481-1484. http://dx.doi.org/10.1126/science.1160787
[8] Trenberth, K.E., Fasullo, J. and Smith, L. (2005) Trends and Variability in Column-Integrated Atmospheric Water Vapor. Climate Dynamic, 24, 741-758.
http://dx.doi.org/10.1007/s00382-005-0017-4
[9] Marengo, J.A., Nobre, C.A. and Tomasella, J. (2008) The Drought of Amazon in 2005. Journal of Climate, 21, 495-516. http://dx.doi.org/10.1175/2007JCLI1600.1
[10] Valipour, M. (2014) Land Use Policy and Agricultural Water Management of the Previous Half of Century in Africa. Applied Water Science. http://dx.doi.org/10.1007/s13201-014-0199-1
[11] Valipour, M., Ahmadi, M.Z., Raeini-Sarjaz, M., Sefidkouhi, M.A.G., Shahnazari, A., Fazlola, R. and Darzi-Naftchali, A. (2014) Agricultural Water Management in the World during Past Half Century. Archives of Agronomy and Soil Science. http://dx.doi.org/10.1080/03650340.2014.944903
[12] Valipour, M. (2012) Critical Areas of Iran for Agriculture Water Management According to the Annual Rainfall. European Journal of Scientific Research, 84, 600-608.
[13] Valipour, M. (2012) Number of Required Observation Data for Rainfall Forecasting According to the Climate Conditions. American Journal of Scientific Research, 74, 79-86.
[14] Marengo, J.A., Borma, L.S., Rodriguez, D.A., Pinho, P., Soares, W.R. and Alves, L.M. (2013) Recent Extremes of Drought and Flooding in Amazonia: Vulnerabilities and Human Adaptation. American Journal of Climate Change, 2, 87-96. http://dx.doi.org/10.4236/ajcc.2013.22009
[15] Marengo, J.A., Javier, T., Alves, L.M., Soares, W.R. and Rodriguez, D.A. (2011) The Drought of 2010 in the Context of Historical Droughts in the Amazon Region. Geophysical Research Letters, 38, L12703.
http://dx.doi.org/10.1029/2011GL047436
[16] Marengo, J.A., Tomasella, J., Soares, W.R., Alves, L.M. and Nobre, C.A. (2012) Extreme Climate Events in the Amazon Basin. Theoretical and Applied Climatology, 107, 73-85.
http://dx.doi.org/10.1007/s00704-011-0465-1
[17] Espinoza, J.C., Ronchail, J., Frappart, F., Lavado, W., Santini, W. and Guyot, J.L. (2012) The Major Floods in the Amazonas River and Tributaries (Western Amazon Basin) during the 1970-2012 Period: A Focus on the 2012 Flood. Journal of Hydrometeorology, 14, 1000-1008.
http://dx.doi.org/10.1175/JHM-D-12-0100.1
[18] Satyamurty, P., da Costa, C.P., Manzi, A.O. and Candido, L.A. (2013) A Quick Look at the 2012 Record Flood in the Amazon Basin. Geophysical Research Letters, 40, 1396-1401.
http://dx.doi.org/10.1002/grl.50245
[19] Fearnside, P.M. (2014) As barragens e as inundações no rio Madeira. Ciência Hoje, 53, 53-57.
[20] Fearnside, P.M. (2014) Impacts of Brazil’s Madeira River Dams: Unlearned Lessons for Hydroelectric Development in Amazonia. Environmental Science and Policy, 38, 164-172.
http://dx.doi.org/10.1016/j.envsci.2013.11.004
[21] Satyamurty, P., de Castro, A.A., Tota, J., da Silva Gularte, L.E. and Manzi, A.O. (2010) Rainfall Trends in the Brazilian Amazon Basin in the Past Eight Decades. Theoretical and Applied Climatology, 99, 139-148. http://dx.doi.org/10.1007/s00704-009-0133-x
[22] Correia, F.W.S., Alvalá, R.C.S. and Manzi, A.O. (2007) Modeling the Impacts of Land Cover Change in Amazônia: A Regional Climate Model (RCM) Simulation Study. Theoretical and Applied Climatology, 93, 225-244.
[23] Sud, Y.C., Chao, W. and Walker, G. (1993) Dependence of Rainfall on Vegetation: Theoretical Considerations, Simulation Experiments, Observations, and Inferences from Simulated Atmospheric Soundings. Journal of Arid Environments, 25, 5-18. http://dx.doi.org/10.1006/jare.1993.1038
[24] Sampaio, G., Nobre, C., Costa, M.H., Satyamurty, P., Soares-Filho, B.S. and Cardoso, M. (2007) Regional Climate Change over Eastern Amazônia Caused by Pasture and Soybean Cropland Expansion. Geophysical Research Letters, 34, LI7709.
[25] Chen, T.C., Takle, J.H. and Yoon, K.J. (2003) Impacts on South America Rainfall Due to Changes in Global Circulation. Proceedings of the 7th International Conference on Southern Hemisphere Meteorology and Oceanography, American Meteorological Society, Boston, 92-93.
[26] Valverde, M. and Marengo, J.A. (2011) Rainfall Extremes Events Climatology over the Amazon Basin. Proceedings of the Global Conference on Global Warming, Lisbon, 11-14 July 2011, 1-8.
[27] Marengo, J.A., Nobre, C.A., Chou, S.C., et al. (2011) Riscos das Mudanças Climáticas no Brasil. Análise Conjunta Brasil-Reino Unido Sobre os Impactos das Mudanças Climáticas e do Desmatamento na Amazônia, 2-56.
[28] Carvalho, L.M., Jones, C. and Liebmann, B. (2003) The South Atlantic Convergence Zone: Intensity, Form, Persistence, and Relationships with Intraseasonal to Interannual Activity and Extreme Rainfall. Journal of Climate, 17, 88-108.
http://dx.doi.org/10.1175/1520-0442(2004)017<0088:TSACZI>2.0.CO;2
[29] Valipour, M. (2014) Future of the Area Equipped for Irrigation. Archives of Agronomy and Soil Science, 60, 1641-1660.
[30] Wheater, H. and Evans, E. (2009) Land Use, Water Management and Future Flood Risk. Land Use Policy, 26, S251-S264. http://dx.doi.org/10.1016/j.landusepol.2009.08.019
[31] Valipour, M. (2014) Future of Agricultural Water Management in Americas. Journal of Agricultural Research, 2, 245-267.
[32] Chou, S.C., Marengo, J.A., Lyra, A.A., Sueiro, G., Pesquero, J.F., Alves, L.M., et al. (2011) Downscaling of South America Present Climate Driven by 4-Member HadCM3 Runs. Climate Dynamics, 38, 635-653.
[33] Collins, M., Tett, F.S.B. and Cooper, C. (2001) The Internal Climate Variability of HadCM3, a Version of the Hadley Centre Coupled Model without Flux Adjustments. Journal of Climate, 17, 61-81.
[34] Gordon, C., Cooper, C., Senior, C.A., Banks, H., Gregory, J.M., Johns, T.C., Mitchell, J.F.B. and Wood, R.A. (2000) The Simulation of SST, Sea Ice Extents and Ocean Heat Transports in a Version of the Hadley Centre Coupled Model without Flux Adjustments. Journal of Climate, 16, 147-168.
[35] Pope, V.D., Gallani, M.L., Rowntree, P.R. and Stratton, R.A. (2000) The Impact of the New Physical Parametrizations in the Hadley Centre Climate Model: HadAM3. Climate Dynamics, 16, 123-146.
http://dx.doi.org/10.1007/s003820050009
[36] Nakicenovic, N., Alcamo, J., Davis, G., et al. (2000) Special Report on Emissions Scenarios, Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, United Kingdom and New York, 599 p.
[37] Black, T.L. (1994) The New NMC Mesoscale ETA Model: Description and Forecast Examples. Weather and Forecasting, 9, 265-278.
http://dx.doi.org/10.1175/1520-0434(1994)009<0265:TNNMEM>2.0.CO;2
[38] Janjié, Z. (1994) The Step-Mountain Eta Coordinate Model: Further Developments of the Convection, Viscous Sublayer, and Turbulance Closure Schemes. Monthly Weather Review, 122, 927-945.
http://dx.doi.org/10.1175/1520-0493(1994)122<0927:TSMECM>2.0.CO;2
[39] Zhao, Q., Black, T.L. and Baldwin, M.E. (1997) Implementation of the Cloud Prediction Scheme in the Eta Model at NCEP. Weather and Forecasting, 12, 697-712.
http://dx.doi.org/10.1175/1520-0434(1997)012<0697:IOTCPS>2.0.CO;2
[40] Chen, F., Janjié, Z. and Mitchell, K. (1997) Impact of Atmospheric Surface-Layer Parameterizations in the New Land-Surface Scheme of the NCEP Mesoscale Eta Model. Boundary-Layer Meteorology, 85, 391-421. http://dx.doi.org/10.1023/A:1000531001463
[41] Ek, M.B., Mitchell, K.E., Lin, Y., Rogers, E., Grunmann, P., Koren, V., Gayno, G. and Tarpley, J.D. (2003) Implementation of NOAH Land Surface Advances in the National Centers for Environmental Prediction Operational Mesoscale Eta Model. Journal of Geophysical Research, 108, 8851.
[42] Sestini, M.F., dos Santos Alvalá, R.C.D., Mello, E.L.K., de Morisson Valeriano, D., Chan, C.S., Nobre, C.A., et al. (2002) Elaboração de mapas de vegetação para utilização em modelos meteorológicos e hidrológicos. INPE, São José dos Campos, 64 p.
[43] Lacis, A.A. and Hansen, J. (1974) A Parameterization of the Absorption of Solar Radiation in Earth’s Atmosphere. Journal of the Atmospheric Sciences, 31, 118-133.
http://dx.doi.org/10.1175/1520-0469(1974)031<0118:APFTAO>2.0.CO;2
[44] Fels, S.B. and Schwarzkopf, M.D. (1975) The Simplified Exchange Approximation: A New Method for Radiative Transfer Calculations. Journal of the Atmospheric Sciences, 32, 1475-1488.
http://dx.doi.org/10.1175/1520-0469(1975)032<1475:TSEAAN>2.0.CO;2
[45] Frich, P., Alexander, L.V., Della-Marta, P., Gleason, B., Haylock, M., Klein Tank, A.M.G. and Peterson, T. (2002) Observed Coherent Changes in Climatic Extremes during the Second Half of the Twentieth Century. Climate Research, 19, 193-212. http://dx.doi.org/10.3354/cr019193
[46] Gao, X., Pal, J.S. and Giorgi, F. (2006) Projected Changes in Mean and Extreme Precipitation over the Mediterranean Region from a High Resolution Double Nested RCM Simulation. Geophysical Research Letters, 33, L03706. http://dx.doi.org/10.1029/2005GL024954

Copyright © 2023 by authors and Scientific Research Publishing Inc.

Creative Commons License

This work and the related PDF file are licensed under a Creative Commons Attribution 4.0 International License.