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Cold fronts and reservoir limnology: an integrated approach towards the ecological dynamics of freshwater ecosystems/Frentes frias e limnologia de reservatorios: uma abordagem integrada para a dinamica ecologica dos ecossistemas de aguas interiores.

1. Introduction

The continuous motion that is a characteristic feature of the pelagic environment is a fundamental forcing function in the spatial and temporal organization of the phytoplanktonic community. Turbulence of various scales sets up the pattern of succession and spatial distribution, and this relationship is now well known (Reynolds, 1997). The vertical structure of turbulent layers depends upon the wind velocity and direction and, the depth of the freshwater ecosystem; the kinetic energy of mixing is opposed by the degree of density stratification. Therefore a continuous process of turbulent mixing and density stratification occurs in lakes and reservoirs promoting a pulse system of fluctuation, that, accordingly to many authors (Harris, 1980, 1986; Padisak, 1993; Padisak et al., 2993) is what influences the species richness, diversity and equitability of phytoplankton in shallow lakes. Evidences of the impact of climatological factors such a precipitation and wind in the southern hemisphere and particularly in Brazil can be found in the literature as early as 1979 (Lima et al., 1979; Tundisi, 1983).

The importance of climatological data for studies in limnology of lakes and reservoirs was stressed by Tundisi et al. (2007) based or earlier work at UHE Carlos Botelho (Lobo/Broa) reservoir that showed strong interactions between wind, precipitation and the seasonal succession of phytoplankton (Tundisi and Matsumura Tundisi, 1995). More recent evidences of the impact of climate on the functioning of reservoirs at southeastern Brazilian given by Branco et al. (2009) emphasized the interactions of climate variables such as wind, air temperature and precipitation with the thermal, chemical and biological structure of the water column at Lages Reservoir (Brazil).

Earlier work on the ecological importance of cold fronts in reservoirs of southern Brazil showed also strong interactions between the passages of the southern air masses and the circulation patterns of reservoirs (Arcifa et al., 1990; Tundisi et al., 2004, 2006).

Barbosa and Padisak (2002) described how atelomixis in lakes and reservoirs is a fundamental process in the daily reorganization of the thermal structure of the water column interacting thus with the phytoplankton vertical distribution and succession in shallow lakes.

In this paper the authors describe with further details and information the impact of cold fronts in freshwater ecosystems of Brazil. This is an attempt to develop and promote an integrated approach and overview of the cold fronts impact in the functioning of reservoirs with the aim to introduce a conceptual framework and the development of a predictive limnological/ecological attitude towards the management of these shallow artificial aquatic ecosystems at southeast Brazil.

2. Material and Methods

2.1. Data collection: literature sources and experimental data

Data from the literature showing vertical distribution of physical variables under the impact of the cold fronts were collected and assembled from many sources in the recent literature (Tundisi et al., 2004, 2006).

Several unpublished results from the laboratories of the International Institute of Ecology of Sao Carlos were also analyzed (Passerini, 2010). These results are part of the project on real time monitoring of physical and chemical variables developed for DERSA (State of Sao Paulo Government), in connection with the monitoring of Billings and Guarapiranga reservoirs. Real time monitoring was performed with a SMARTER plataform and satellite transmission of data (Patent deposited IIE).

Recent data from papers on the ecological dynamics of a shallow reservoir (Tundisi et al., 2008a) and the climatology of cold fronts on the Metropolitan region of Sao Paulo are also analyzed (Morais et al., 2010).

2.2 Analysis of cold fronts frequencies and variability in South America

The results and data presented by Cavalcanti and Kousky (2009) are summarized as a basic information for the cold front--reservoir limnology case study. The data for South Eastern Brazil presented by these authors is discussed.

2.3. The dynamics of the cold fronts in the South American continent and the Southeast Brazil

Accordingly with Cavalcanti and Kousky (2009), there is seasonality in the occurrence of the cold fronts passage in the South American continent. The cold fronts are more frequent from May to September and less frequent during the summer in the southern hemisphere between the latitudes 25[degrees] and 30[degrees], cold fronts occur during all year round but in greater number from May to October.

Figure 1 shows the average number of cold fronts from 1980 to 2002. For comparative purposes the monthly regime of cold fronts in the metropolitan region of Sao Paulo is shown in Figure 2.

For the southeast region of Brazil, Cavalcanti and Kousky (2009) showed a yearly frequency of 50 to 60 cold fronts. Also these authors demonstrated an excellent relationship between the cold fronts and the atmospheric variables such as air temperature, (lower air temperatures) increase of atmospheric pressure at sea level, and increase in wind velocity. Also an effect on the intensity and distribution of precipitation occurs. An increase in the precipitation is typical during the passage of cold fronts. Figure 3 shows a typical progression of cold fronts in the southeast Brazil. The dynamics of the process last for hours to lays accordingly with the existing data.

3. Results

Figure 4 shows the changes during the cold fronts in Barra Bonita reservoir related to the vertical structure of the water column, temperature and stability (Tundisi et al., 2006) and thermal resistence to circulation.

Figure 5 shows the same reservoir under the effects of the cold front.



Figure 6a shows the vertical structure of the water column at Billings reservoir during December 2007. The presence of the cold fronts is indicated. Periods of stratification and stability, work of the wind and thermal resistance to circulation during the same period are shown. The system repeats in March 2008 of the same station in Billings reservoir; low stability and low thermal resistance to circulation related to the cold fronts effects (Figure 7a and 7b).

Caraballo et al. (2010, in press) observed and reported the impact of a cold front ("friagem") in May 2006 in lake Catalao located at the confluence of the Negro river and Solimoes river in front of the city of Manaus (3[degrees]10'04"S and 59[degrees]54'45"W). On the second day of the "friagem" accordingly to these authors, the 12 meter water column of the lake was completely mixed with a temperature of 27,8[degrees]C. Low levels of oxygen in the water near the surface of the lake were found as a consequence of destratification and mixing coupled with the "friagem" event and impact. The cold front impact caused a significant temperature difference during the nictimeral cycle. During this event hydrogen sulfide gas and dead fish were not found. However in other episodes of cold fronts this is a common feature in Amazonian and Pantanal floodplain lakes (Fearnside, 1995;). Surface cooling and strong density currents promoting complete mixing even in lakes deeper than 10 meters were reported by Tundisi et al. (1984); Melack and Fisher (1990).

In conclusion, all the existing experimental evidence and literature sources show a strong effect of cold fronts in reservoirs of southeast Brazil and in Amazon and Pantanal lakes. These sources, clearly demonstrated that cold fronts are a significant forcing function coupled with climatic variation that affects these freshwater ecosystems at a wide range of latitudes in South America.


4. Discussion

There is now strong evidence that cold fronts are a fundamental forcing function in the mixing of reservoirs and natural lakes mainly in the southeast Brazil and at Amazonian and Pantanal lakes.

The vertical and horizontal mixing that takes place after the passage of cold fronts has impacts and consequences on the phytoplankton succession and in the mixing patterns of the freshwater ecosystems.

When cold fronts are operating in full scale the cooling of the surface waters and the vertical mixing changes the thermal structure of lakes and reservoirs producing homogeneous profiles of water temperature, dissolved oxygen, electrical conductivity of the water and nutrients, such as phosphorus and nitrogen (Tundisi et al., 2004, 2006; Branco et al., 2009; Morais et al., 2010; Caraballo et al., 2010).


Cold fronts originating in southern South America present a seasonal variation as demonstrated by Cavalcanti and Kousky (2009), and discussed by Morais et al. (2010).

In an environment characterized by reduced wind impact there is a lack of mixing and predominance of cyanobacteria blooms of the surface and subsurface of the water column. Tundisi (1983) demonstrated that for reservoirs of the Tiete river in Sao Paulo State growth and prevalence of cyanobacteria blooms are depending on the stability of the water column, the average depth of the stratified column and the radio N:P. During periods of stability of the water column the mixed layer is depleted of nutrients very rapidly therefore phytoplankton should depends on the nutrient regeneration and the ability of cyanobacterias to fix nitrogen. Increase of ammonia in the stratified layer due to zooplankton excretion is another possible source of nitrogen regeneration (Tundisi, 1983).

Intense turbulence immediately before and during the cold fronts establishes the mixing in the vertical and horizontal scales promoting the growth of chlorophyceae and diatoms during these short periods of 2 or 3 days.

Harris et al. (1986) emphasized the effect of physical factors in the control of phytoplankton dynamics and discussed the time scales of physical fluctuations coupled with the response of the phytoplanktonic community. Several authors demonstrated the response of the phytoplankton related to the extent and degree of vertical turbulence (Ganf, 1974; Reynolds, 1997). The ratio of the euphotic zone (Zeu) to the depth of the mixed layer (Zmix) is a fundamental physical component, of critical depth models as shown by Harris (1980).

Turbulence promoted by cold fronts changes very rapidly this ratio Zeu/Zmix therefore physiological adaptation of the phytoplankton to these short time changes can be expected. But besides these physiological adaptations, the physical forcing functions promoted by turbulence before and during the cold fronts changes the succession patterns of phytoplankton; changes in the growth rates of phytoplankton due to varying nutrient concentration may be expected also (William and Goldman, 1975).


Tundisi et al. (2008a) showed how the patterns of phytoplankton succession changes at Barra Bonita reservoir during alternating periods of cold front impacts and stability of the water column. Wind velocities, frequency of cold fronts and cyanobacteria dominance were shown for this reservoir. The horizontal scale changes with the system being decomposed as horizontal heterogeneous units with a non uniform distribution of zooplankton, phytoplankton and bacteria (Tundisi et al., 2008a). The seasonal pattern of variation of the Wedderburn number confirms the successional patterns of the phytoplankton community. At higher Wedderburn number and low wind force cyanobacteria blooms predominate in the surface or subsurface of the reservoir (Tundisi and Matsumura Tundisi, 2008).

The interaction of solar radiation, water and wind regimes influence the cycles of events in the vertical structure of the freshwater ecosystems at tropical and subtropical latitudes (Talling, 1969; Talling and Lemoalle, 1998). Wind seasonality is an important interacting factor as well as the surface cooling that occur during the duration of cold fronts. Wind affects suspended particulate material, turbidity, living and non living planktonic material therefore the cold front introduce a certain irregularity of factor variations. Its impact is dependent upon the duration of the process, the depth of the freshwater ecosystem and its latitude. The impact of precipitation during the cold fronts also, cannot be disregarded. Precipitation can discharge nutrients by drainage introducing the "new nutrient component" to the lake or reservoir, therefore increasing the pool of nutrients available to phytoplankton growth. A strong effect of the cold front, not so common, dependent upon the duration of the phenomenon and the strength of the winds is the fish mortality in some lakes or shallow reservoirs at various latitudes.



Considering now the existing information, it is possible to propose a mechanism of functioning of reservoirs and lakes of southeastern Brazil related to the patterns of cold fronts/instability and absence of cold fronts/stability (Table 1).

This table is based on Demers et al. (1951), Reynolds (1997), Tundisi et al. (2004) and Branco et al. (2009). It is an attempt to propose a model of phytoplankton succession for lakes and reservoirs based on the instability of the water column and the absence or presence of the cold front. The prediction of the frequency of cyanobacteria blooms is one of the best possibilities of application since enables water managers to organize and prepare water treatment accordingly to the water quality at the source of supply.

Since cold fronts contribute towards deterioration of the water quality for public supply, the follow up of the impact of the cold fronts is a fundamental priority (Tundisi et al., 2008b).

Acknowledgements--The authors thank FAPESP, CNPQ, FINEP for many years of support for their reservoir ecosystem work. The author thank the Secretaria do Verde e Meio Ambiente, Prefeitura Municipal de S. Paulo-Process number: 056/ SVMA/ 2008 for the support to their work in the Guarapiranga/ Billings reservoirs. Also the support of DERSA (Government of S. Paulo State) is gratefully acknowledged. Biota FAPESP supported field work.


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Tundisi, JG. (a) *, Matsumura-Tundisi, T. (a), Pereira, KC. (a), Luzia, AP. (a), Passerini, MD. (a), Chiba, WAC. (a), Morais, MA. (a) and Sebastien, NY. (b)

(a) Instituto Internacional de Ecologia--IIE, Rua Bento Carlos, 750, Centro, CEP 13560-660, Sao Carlos, SP, Brazil

(b) Centro de Ciencias Exatas e Tecnologicas, Universidade Estadual do Oeste do Parana--UNIOESTE, Rua da Faculdade, 645, Jardim La salle, CP 520, CEP 85903-000, Toledo, PR, Brazil

* e-mail:

Received January 08, 2010--Accepted June 05, 2010--Distributed October 31, 2010 (With 7 figures)
Table 1. Phytoplankton responses to cold fronts through the
proximal agent vertical mixing or stability.

Cold fronts                Proximal agent         Phytoplankton

1) No cold fronts          No vertical or        Cyanobacterial
                         horizontal mixing;          blooms.
                        nutrients available
                            only through
2) Moderate vertical    Alternating periods      Cyanobacterial
  mixing previous         of stability and       blooms start to
  cold front                  mixing.              break down.
                                                  Selection for
                                                 chlophyceae and
                                                 small diatoms.
3) Cold front              Changing light          Diatoms and
                       environment. Nutrients     chlorophyceae
                            continuously          predominate.
                            Vertical and
                         horizontal mixing
                          (very intense).
4) Cold front            Beginning of a new       Beginning of
  dissipates            cycle of stability.      cyanobacterial
                       Increase of light and       growth. Pre
                          nutrients in the      bloom conditions.
                           stable layer.
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Author:Tundisi, J.G.; Matsumura-Tundisi, T.; Pereira, K.C.; Luzia, A.P.; Passerini, M.D.; Chiba, W.A.C.; Mo
Publication:Brazilian Journal of Biology
Date:Aug 1, 2010
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