TIP 4 Brazilian programs | |||||
Brazilian
Ocean-Climate programs Seasonal Climate Prediction at CPTEC/INPE
Ocean-atmosphere interactions over the tropical Atlantic: Interannual climate variability over the tropical Atlantic is dominated by anomalous meridional migrations of the intertropical convergence zone (ITCZ). It is shown that modulation of ITCZ migrations are related to modulations of meridional gradients of anomalous SST over the tropical Atlantic. Also, it is shown that rainfall anomalies that affect Nordeste (Northeast Brazil) are large scale phenomenon, encompassing the whole equatorial Atlantic and eastern Amazon region. Observational evidence supports the conjecture that atmospheric dynamics, linked to the occurrence of teleconnnection patterns originating from the equatorial central Pacific modulate the formation of anomalous SST patterns over northern tropical Atlantic. It is suggested that an ocean-atmosphere observing system over the tropical Atlantic must go beyond the equatorial band to be useful for seasonal rainfall forecasting over Brazil. Seasonal Climate forecasting at CPTEC: The numerical seasonal rainfall forecast experiment done at CPTEC for the March April May (MAM) 1995 rainy season over northeast Brazil (Nordeste) is described. The model used is COLA/CPTEC's AGCM (T62 L28). Four member ensembles with varying initial conditions are used to obtain the seasonal forecasts. For each initial condition the AGCM is integrated for six months for both climatological and forecasted SSTs. Persisted SST anomalies are used to simulate forecasted SSTs. The runs which used persisted December 1994 SST anomalies (while ENSO conditions still dominated over the equatorial Pacific), forecasted MAM negative rainfall anomalies over Nordeste, in disagreement with the observed positive anomalies. The next runs, which used January, February, and March persisted SST anomalies respectively, showed progressively better forecasts, as the monthly SST fields approached more and more the actual MAM SST. The differences between the December and January forecasts (with the latter showing closer-to-observed values), are attributed in large part to the more favorable SST conditions over the southern tropical Atlantic in January, since not much change occurred over the equatorial Pacific during that period. These results highlight the importance of forecasting tropical Atlantic SST for the seasonal rainfall numerical predictions over the Nordeste, the equatorial Atlantic, and the Amazon regions. A March 1995 persisted SST anomaly run generated MAM rainfall forecast that resembled closely the observed rainfall distribution (Figure 5). It is concluded that atmospheric general circulation modeling is capable of predicting seasonal rainfall anomalies over Nordeste, provided accurate SST fields are prescribed. For the December 1994 March 1995 period, persisting SST anomalies was shown to be a poor method of forecasting SSTs over the tropical Atlantic and equatorial Pacific. Atlantic Ocean Processes, Ocean Observing Systems and the Predictability of Fluctuations in Climate and Fisheries Yields at Seasonal to Interdecadal Scales M. Vianna, INPE, Brazil We review here some basic and distinct features of the large-scale air-sea interaction and ocean circulation in the Atlantic tropics and subtropics, which have to be monitored in order to support to the development of realistic coupled circulation models that may be used for regional climate prediction at several scales. This is done to give insight into the formulation of criteria to prioritize the siting of elements of an Atlantic TAO Ocean Observing System in certain key regions. Among the distinct features, we will concentrate on our studies of the Atlantic high-resolution SSTA (SST anomaly) dynamics (Vianna and Kampel, 1995), which seem to imply Rossby wave-driven westward spread of SSTA's, and the following:
References: Carton, J.A. and B.Huang, 1994: Warm events in the Tropical Atlantic. J. Phys. Oceanogr. 24, 888 903. Delecluse, P., J. Servain, C. Levy, K. Arpe, and L. Bengtsson, 1994: On the connection between the 1984 Atlantic warm event and the 1982-1983 ENSO. Tellus, 46A, 448-464. Houghton, R.W. 1991: The relationship of Sea Surface Temperature to thermocline depth at annual and interannual time scales in the tropical Atlantic ocean. J. Geophys. Res., 96(C8), 15:173 15:185. Kawamura, R. 1994: A rotated EOF analysis of global sea surface temperature variability with interannual and interdecadal scales. J. Phys. Oceanogr., 24, 707-715. Molinari, R. L. 1982: Observations of eastward currents in the tropical south Atlantic ocean: 1978 1980. J. Geophys. Res., 87(C12), 9707-9714. Schott, F.A. and C.W. Boning, 1991: The WOCE model in the western Equatorial Atlantic: upper layer circulation. J. Geophys.Res., 96(C4), 6993-7004. Servain, J.M., A. Morliere, C.S. Pereira, 1994: Simulated versus observed sea surface temperature in the tropical Atlantic Ocean. The Global Atm. Ocean Sys., 2, 1-20. Tourre, Y.M. and W.B. White, 1995: ENSO signals in global upper ocean temperature. J. Phys. Oceanogr., 6, 1317-1332. Vianna, M.L. and M. Kampel, 1995: A high resolution study of the dynamics of Atlantic SST fields. In: Proc. TOGA 95 International Scientific Conference, 2-7 April 1995, Melbourne, Australia (to appear as a WMO Publication).
Status of Brazilian
Anchored and Drifting Buoys FUNCEME's Programs
(Present and Planned) in Climate Studies The east part of the Northeast has its rainy season between May and August. In contrast, the characteristic regime of the southern part of the region has maximum precipitation in November/December. The Northern part of the Northeast (Nordeste) is known for its semi-arid climate with its rainy season concentrated between February and May, and very large interannual variability that can vary from 50% through 150% of the average. Many authors have identified the relationship between precipitation over the Northeast and ENSO events; Atlantic Ocean sea surface temperature, trade winds, and sea level pressure; the position of the Intertropical Convergence Zone (ITCZ) over the Atlantic Ocean; cold fronts and other phenomena. The Nordeste not only exhibits a high variability in the total amount of precipitation from year to year but also, a high spatial and temporal variability in the precipitation within its rainy season. This monthly variability is related to the different rainfall systems that cause precipitation over the region in the different months of the rainy season. February and March is the period when the ITCZ over Tropical Atlantic Ocean reaches its southern most position, initializing what is called the principal' rainy season over Nordeste. The return of the ITCZ to its more northern position is what determines the end of the Nordeste principal rainy season. Some mechanisms of the ITCZ movement are related to the thermal conditions over either the Pacific or the Atlantic Basins. Recent work has shown that both oceans have influences on Nordeste precipitation during the different months of the rainy season. However, it seems that sea surface temperature (SST) anomalies in the Atlantic Ocean are more important than those in the Pacific in controlling the precipitation variability of the Nordeste. The high interannual variability and the high spatial and temporal distribution of the precipitation have enormous impacts on the society and economy of the region generating population migration and high level of unemployment. Different methodologies have been developed to forecast the Nordeste's rainy season and have been used during the last several years for operational purposes at the National Institute for Space Research-INPE in Sao Jose dos Campos - SP - Brazil and at the Ceara State Foundation for Meteorology and Water Resources (FUNCEME). Those methodologies are based on empirical atmospheric and oceanic parameters, on results from coupled models and on statistical models, developed specifically for forecasting Nordeste rainy season. The predictability of the quality of the rainy season has great importance for local agriculture and the water management of the region. The main users of the climate information generated by FUNCEME are farmers, civil defense, insurance companies, banks, press, water management company, and the agricultural secretariat, which has a special program for seed distribution. As the Atlantic Basin is very important to the climate variability of the region, some projects related to it are under development at FUNCEME, e.g., a dynamical-stochastic model for monthly SST anomalies (in collaboration with a senior scientist from Hydro-meteorological Center of Moscow-Russia), Canonical Correlation Analysis model and SST retrieval by using NOAA/AVHRR data. A new TAO array over the Atlantic Basin will improve the quality of observational data over the basin. It will also contribute to studies related to Nordeste climate variability as well as help validate SST retrievals from satellite imagery, with applications for climate monitoring, climate modeling and fishery activities. |
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