Wind speed trends over the southwestern Atlantic Ocean, between 33° and 50°S
Surface scalar wind speed trends (from 1979 to 2009) at the southwestern Atlantic Ocean, between 33° and 50°S and 55° and 70°W, were estimated from the NCEP/NCAR I (NR1) and the Climate Forecast System Reanalysis (CFSR) using Sen's slope. Trends were tested using the seasonal Mann-Kendall test....
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| Formato: | Capítulo de libro |
| Lenguaje: | Inglés |
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John Wiley and Sons Ltd
2016
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| Acceso en línea: | Registro en Scopus DOI Handle Registro en la Biblioteca Digital |
| Aporte de: | Registro referencial: Solicitar el recurso aquí |
| LEADER | 11669caa a22011537a 4500 | ||
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| 001 | PAPER-24564 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205626.0 | ||
| 008 | 190411s2016 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-84958062370 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 030 | |a IJCLE | ||
| 100 | 1 | |a Pescio, A.E. | |
| 245 | 1 | 0 | |a Wind speed trends over the southwestern Atlantic Ocean, between 33° and 50°S |
| 260 | |b John Wiley and Sons Ltd |c 2016 | ||
| 270 | 1 | 0 | |m Dragani, W.C.; Oceanografía, Servicio de Hidrografía Naval, Ministerio de Defensa, Av. Montes de Oca 2124, Argentina; email: dragani@hidro.gov.ar |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a Surface scalar wind speed trends (from 1979 to 2009) at the southwestern Atlantic Ocean, between 33° and 50°S and 55° and 70°W, were estimated from the NCEP/NCAR I (NR1) and the Climate Forecast System Reanalysis (CFSR) using Sen's slope. Trends were tested using the seasonal Mann-Kendall test. Scalar wind speed trends computed from NR1 database were positive throughout the whole study area, with values ranging from +0.01 to +0.03 m s-1 year-1. On the contrary, wind speed trends computed from CFSR database were rather different to trends obtained from NR1 reanalysis. Wind speed and sea surface temperature (SST) trend patterns, both computed from CFSR database, seem to be quite consistent but, in general, no apparent relationship between both patterns was obtained when different global databases were analysed. Sea surface wind speed data compiled from multiple satellite observations were also used to compute wind speed trends. Computed satellite trends resulted in very good agreement with positive values obtained from NR1 database. NR1 data series presented significant inter-annual to multi-decadal oscillations at the Argentinean continental shelf, but they would not seem to be associated either with the Southern Annular Mode or with El Niño Southern Oscillation. Possible impacts of positive speed wind trends on the mean depth of the ocean mixed layer and on the wind wave climate are briefly discussed. © 2016 Royal Meteorological Society. |l eng | |
| 593 | |a Oceanografía, Servicio de Hidrografía Naval, Ministerio de Defensa, Ciudad Autónoma de Buenos Aires, Argentina | ||
| 593 | |a Departamento de Ciencias de la Atmósfera y los Océanos, UMI IFAECI/CNRS - CONICET-UBA, Ciudad Universitaria, Ciudad Autónoma de Buenos Aires, Argentina | ||
| 593 | |a CONICET, Consejo Nacional de Investigaciones Científicas y Técnicas, Ciudad Autónoma de Buenos Aires, Argentina | ||
| 690 | 1 | 0 | |a ARGENTINEAN CONTINENTAL SHELF |
| 690 | 1 | 0 | |a GLOBAL REANALYSIS |
| 690 | 1 | 0 | |a SATELLITE DATA |
| 690 | 1 | 0 | |a SOUTHWESTERN ATLANTIC OCEAN |
| 690 | 1 | 0 | |a WIND SPEED TREND |
| 690 | 1 | 0 | |a ATMOSPHERIC PRESSURE |
| 690 | 1 | 0 | |a ATMOSPHERIC TEMPERATURE |
| 690 | 1 | 0 | |a DATABASE SYSTEMS |
| 690 | 1 | 0 | |a OCEAN CURRENTS |
| 690 | 1 | 0 | |a OCEANOGRAPHY |
| 690 | 1 | 0 | |a SATELLITES |
| 690 | 1 | 0 | |a SPEED |
| 690 | 1 | 0 | |a SURFACE WATERS |
| 690 | 1 | 0 | |a CONTINENTAL SHELVES |
| 690 | 1 | 0 | |a REANALYSIS |
| 690 | 1 | 0 | |a SATELLITE DATA |
| 690 | 1 | 0 | |a SOUTHWESTERN ATLANTIC OCEAN |
| 690 | 1 | 0 | |a WIND SPEED |
| 690 | 1 | 0 | |a WIND |
| 690 | 1 | 0 | |a CONTINENTAL SHELF |
| 690 | 1 | 0 | |a EL NINO-SOUTHERN OSCILLATION |
| 690 | 1 | 0 | |a SATELLITE DATA |
| 690 | 1 | 0 | |a SEA SURFACE TEMPERATURE |
| 690 | 1 | 0 | |a TREND ANALYSIS |
| 690 | 1 | 0 | |a WEATHER FORECASTING |
| 690 | 1 | 0 | |a WIND VELOCITY |
| 690 | 1 | 0 | |a ARGENTINE SHELF |
| 690 | 1 | 0 | |a ATLANTIC OCEAN |
| 690 | 1 | 0 | |a ATLANTIC OCEAN (SOUTHWEST) |
| 700 | 1 | |a Martin, P.B. | |
| 700 | 1 | |a Dragani, W.C. | |
| 773 | 0 | |d John Wiley and Sons Ltd, 2016 |g v. 36 |h pp. 501-507 |k n. 1 |p Int. J. Climatol. |x 08998418 |w (AR-BaUEN)CENRE-40 |t International Journal of Climatology | |
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| 856 | 4 | 0 | |u https://doi.org/10.1002/joc.4348 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_08998418_v36_n1_p501_Pescio |y Handle |
| 856 | 4 | 0 | |u https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08998418_v36_n1_p501_Pescio |y Registro en la Biblioteca Digital |
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