Further evidence of changes in the hydrological regime of the River Paraguay: part of a wider phenomenon of climate change?

Citation
W. Collischonn et al., Further evidence of changes in the hydrological regime of the River Paraguay: part of a wider phenomenon of climate change?, J HYDROL, 245(1-4), 2001, pp. 218-238
Citations number
30
Categorie Soggetti
Environment/Ecology,"Civil Engineering
Journal title
JOURNAL OF HYDROLOGY
ISSN journal
00221694 → ACNP
Volume
245
Issue
1-4
Year of publication
2001
Pages
218 - 238
Database
ISI
SICI code
0022-1694(20010501)245:1-4<218:FEOCIT>2.0.ZU;2-9
Abstract
Analysis of flow measured at 20 sites, rainfall measured at 36 sites, and a 95-year record of water-le vel at one site in the basin of the River Parag uay (area 1095 x 10(3) km(2)) showed that the flow regime during the approx imate period 1960-1970 differed substantially from the flow regime both bef ore and after. The long record of Ladario water-levels suggested that the c hanges between one period and the next were considerably abrupt, and that t he periods differed not only in terms of mean water-levels but also in term s of the year-to-year correlational structure within the record. Despite th e fragmentary nature of rainfall records from 36 sites, an explanation for the increased hows since 1970 was found in the increases of rainfall, as as sessed in terms of the frequency of annual rainfalls more than the long-ter m mean rainfall. There was some degree of consistency in the change of rain fall pattern across the Paraguay basin as a whole. A detailed examination o f daily rainfall characteristics at two gauges where records were fairly co mplete showed that during the 1960-1970 period, when river flows were low, dry spells were more persistent and, on days when rain did fall, the amount s of rain were generally smaller. The results obtained were compared with r esults obtained by other researchers using flow records from the Rivers Par aguay, Parana, Negro and Uruguay in the la Plata basin, and rainfall record s from other parts of South America There is now strong evidence of changes in the runoff regime of the la Plata basin during the last 40 years, not a ll of which can be attributed to land-use change, as there is complementary evidence of change in rainfall regime. The results were also compared with findings from the Congo basin, which appears to exhibit changes in flow re gime that are a mirror image of those found for the Paraguay at Ladario. (C ) 2001 Elsevier Science B.V. All rights reserved.