Spatiotemporal structures of rainfall over the Amazon basin derived from TRMM data
On the basis of Tropical Rainfall Measuring Mission (TRMM) daily accumulated rainfall data (3B42 v7 product) covering 16 years (1998-2013), the Amazon Basin (AB) time and space rainfall variability is analysed. Different behaviours of precipitation over AB are found to the north and south of 8°S whe...
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John Wiley and Sons Ltd
2016
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| LEADER | 09731caa a22009497a 4500 | ||
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| 001 | PAPER-24504 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205622.0 | ||
| 008 | 190411s2016 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84937622234 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 030 | |a IJCLE | ||
| 100 | 1 | |a Hierro, R. | |
| 245 | 1 | 0 | |a Spatiotemporal structures of rainfall over the Amazon basin derived from TRMM data |
| 260 | |b John Wiley and Sons Ltd |c 2016 | ||
| 270 | 1 | 0 | |m Hierro, R.; Facultad de Ingeniería, Universidad Austral, Mariano Acosta 191, Argentina; email: rhierro@austral.edu.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Buarque, D.C., de Paiva, R.C.D., Clarke, R.T., Mendes, C.A.B., A comparison of Amazon rainfall characteristics derived from TRMM, CMORPH and the Brazilian national rain gauge network (2011) J. Geophys. Res., 116, p. D19105 | ||
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| 504 | |a Clarke, R.T., Buarque, D.C., de Paiva, R.C.D., Collischonn, W., Issues of spatial correlation arising from the use of TRMM rainfall estimates in the Brazilian Amazon (2011) Water Resour. Res., 47, p. W05539 | ||
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| 504 | |a Figueroa, S.N., Nobre, C.A., Precipitation distribution over central and western tropical South America (1990) Climanalise, 5, pp. 36-45 | ||
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| 504 | |a Marengo, J.A., Interdecadal variability and trends of rainfall across the Amazon basin (2004) Theor. Appl. Climatol., 78, pp. 79-96 | ||
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| 504 | |a Nair, S., Srinivasan, G., Nemani, R., Evaluation of multi-satellite TRMM derived rainfall estimates over a western state of India (2009) J. Meteorol. Soc. Jpn., 87, pp. 927-939 | ||
| 504 | |a Nobre, C.A., Oyama, M.D., Oliveira, G.S., Marengo, J.A., Salati, E., Impacts of climate change scenarios for 2091-2100 on the biomes of South America (2004), First CLIVAR International Conference, Baltimore, MD, 21-25 June; Nobre, C.A., Obregón, G.O., Marengo, J.A., Fu, R., Poveda, G., Characteristics of Amazonian climate: main features (2009) Amazonia and Global Change, , Keller M, Bustamante M, Gash J, Silva Dias P (eds). American Geophysical Union: Washington, DC | ||
| 504 | |a de Paiva, R.C.D., Buarque, D.C., Clarke, R.T., Collischonn, W., Allasia, D.G., Reduced precipitation over large water bodies in the Brazilian Amazon shown from TRMM data (2011) Geophys. Res. Lett., 38, p. L04406 | ||
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| 504 | |a Tanaka, LM., Satyamurty, P., Machado, L.A.T., Diurnal variation of precipitation in central Amazon Basin (2014) Int. J. Climatol., 34, pp. 3574-3584 | ||
| 504 | |a Torrence, C., Compo, G.P., A practical guide to wavelet analysis (1998) Bull. Am. Meteorol. Soc., 79, pp. 61-78 | ||
| 504 | |a Valens, C., A really friendly guide to wavelets (1999), http://perso.wanadoo.fr/polyvalens/clemens/wavelets/wavelets.html, (current June 19th, 2015); Yi, H., Shu, H., The improvement of the Morlet wavelet for multi-period analysis of climate data (2012) Comptes Rendus Geosci., 344, pp. 483-497 | ||
| 504 | |a Zhao, T., Yatagai, A., Evaluation of TRMM 3B42 product using a new gauge-based analysis of daily precipitation over China (2014) Int. J. Climatol., 34, pp. 2749-2762 | ||
| 520 | 3 | |a On the basis of Tropical Rainfall Measuring Mission (TRMM) daily accumulated rainfall data (3B42 v7 product) covering 16 years (1998-2013), the Amazon Basin (AB) time and space rainfall variability is analysed. Different behaviours of precipitation over AB are found to the north and south of 8°S when the longitudinal band 70°-50°W is considered. The sample is then split into northern and southern sectors with respect to 8°S, describing their monthly evolution as a function of longitude. The main spatial oscillation modes are isolated and analysed through continuous wavelet transform analysis. Intense spatial oscillations are found close to the western side of the studied region. Several temporal modes in different scales are detected within each sample. Two of them show scales longer than 12 months, which are probably associated with ENSO phases. Smaller scale oscillations, evaluated from daily data, are also found. The northern sector of AB shows more daily data variability than the southern one and seems to be more affected by large temporal processes than the southern sector. © 2016 Royal Meteorological Society. |l eng | |
| 593 | |a Facultad de Ingeniería, Universidad Austral, Pilar, Argentina | ||
| 593 | |a Instituto de Física de Buenos Aires (IFIBA), Buenos Aires, Argentina | ||
| 651 | 4 | |a SOUTH AMERICA RAINFALL | |
| 651 | 4 | |a SOUTH AMERICA | |
| 690 | 1 | 0 | |a TRMM |
| 690 | 1 | 0 | |a WAVELET |
| 690 | 1 | 0 | |a CLIMATOLOGY |
| 690 | 1 | 0 | |a RAIN GAGES |
| 690 | 1 | 0 | |a WAVELET TRANSFORMS |
| 690 | 1 | 0 | |a ACCUMULATED RAINFALL |
| 690 | 1 | 0 | |a CONTINUOUS WAVELET TRANSFORM |
| 690 | 1 | 0 | |a RAINFALL VARIABILITY |
| 690 | 1 | 0 | |a SPATIO-TEMPORAL STRUCTURES |
| 690 | 1 | 0 | |a TRMM |
| 690 | 1 | 0 | |a TROPICAL RAINFALL MEASURING MISSIONS |
| 690 | 1 | 0 | |a WAVELET |
| 690 | 1 | 0 | |a RAIN |
| 690 | 1 | 0 | |a PRECIPITATION ASSESSMENT |
| 690 | 1 | 0 | |a RAINFALL |
| 690 | 1 | 0 | |a SPATIOTEMPORAL ANALYSIS |
| 690 | 1 | 0 | |a TRMM |
| 690 | 1 | 0 | |a WAVELET ANALYSIS |
| 690 | 1 | 0 | |a AMAZON BASIN |
| 700 | 1 | |a Llamedo, P. | |
| 700 | 1 | |a de la Torre, A. | |
| 700 | 1 | |a Alexander, P. | |
| 773 | 0 | |d John Wiley and Sons Ltd, 2016 |g v. 36 |h pp. 1565-1574 |k n. 3 |p Int. J. Climatol. |x 08998418 |w (AR-BaUEN)CENRE-40 |t International Journal of Climatology | |
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