The marshes have a system of diffuse runoff that functions on three different levels
(surface, intermediate and deep), and the marginal swamps toward the lakes and
channels, in an overall northeast-southwest sense, usually determine the orientation
of the movement of the water to empty finally into the Middle Parana through the Río
Corriente. The water balance is favourable to the permanence of water, favoured by
autumn rains and low winter temperatures, which reduce the effect of
evapotranspiration.
The marshes have a system of diffuse runoff that functions on three different levels(surface, intermediate and deep), and the marginal swamps toward the lakes andchannels, in an overall northeast-southwest sense, usually determine the orientationof the movement of the water to empty finally into the Middle Parana through the RíoCorriente. The water balance is favourable to the permanence of water, favoured byautumn rains and low winter temperatures, which reduce the effect ofevapotranspiration.
การแปล กรุณารอสักครู่..