TY - JOUR
T1 - Cambios en la precipitación de la ciudad de Valdivia (Chile) durante los últimos 150 años
AU - González-Reyes, Álvaro
AU - Muñoz, Ariel A.
PY - 2013
Y1 - 2013
N2 - Extensive records of rainfall are considered fundamental for analysing potential current climate change especially in zones where ecosystems are highly humidity dependent. Valdivia city has the longest instrumental record in the nation, starting in 1853, though including a lapse between 1880 and 1899. The present study had the main objective of evaluating changes in precipitation in annual, seasonal and monthly periods and distribution extreme values from 1901 to 2005; further, the activity of global scale climate forcing, such as ENSO and AAO, over the precipitation. Additionally, we have filled this gap period with other instrumental historical registers and Araucaria araucana Tree Ring chronology by evaluated rainfall shifts since 1853. Annual, seasonal and monthly decreases were registered betwee 1901 and 2005. Especially significant for 1853 - 2005, 1901 - 2005, autumn and September. Negative extreme values (droughts) were more frequent in the second half-century, compared with positive extreme values obtained prior to 1950. A high concentration of negative values was also registered post-1980, especially in autumn and winter. Significant and negative correlations were registered between the SOI indexes of ENSO, with a strong relationship across the year, except in summer. The AAO has registered negative and significant relationships as well, particularly during autumn, and February and March. These decreases suggest an extension of summer-time conditions in Valdivia for longer intervals, concentrating precipitation in winter.
AB - Extensive records of rainfall are considered fundamental for analysing potential current climate change especially in zones where ecosystems are highly humidity dependent. Valdivia city has the longest instrumental record in the nation, starting in 1853, though including a lapse between 1880 and 1899. The present study had the main objective of evaluating changes in precipitation in annual, seasonal and monthly periods and distribution extreme values from 1901 to 2005; further, the activity of global scale climate forcing, such as ENSO and AAO, over the precipitation. Additionally, we have filled this gap period with other instrumental historical registers and Araucaria araucana Tree Ring chronology by evaluated rainfall shifts since 1853. Annual, seasonal and monthly decreases were registered betwee 1901 and 2005. Especially significant for 1853 - 2005, 1901 - 2005, autumn and September. Negative extreme values (droughts) were more frequent in the second half-century, compared with positive extreme values obtained prior to 1950. A high concentration of negative values was also registered post-1980, especially in autumn and winter. Significant and negative correlations were registered between the SOI indexes of ENSO, with a strong relationship across the year, except in summer. The AAO has registered negative and significant relationships as well, particularly during autumn, and February and March. These decreases suggest an extension of summer-time conditions in Valdivia for longer intervals, concentrating precipitation in winter.
KW - Antarctic Oscillation AAO
KW - Autumn precipitation
KW - El Niño Southern Oscillation ENSO
KW - Extreme values
KW - Valdivian ecoregion
UR - http://www.scopus.com/inward/record.url?scp=84885735136&partnerID=8YFLogxK
U2 - 10.4067/S0717-92002013000200008
DO - 10.4067/S0717-92002013000200008
M3 - Article
AN - SCOPUS:84885735136
VL - 34
SP - 191
EP - 200
JO - Bosque
JF - Bosque
SN - 0304-8799
IS - 2
ER -