Journal
ISOTOPES IN ENVIRONMENTAL AND HEALTH STUDIES
Volume 52, Issue 1-2, Pages 128-140Publisher
TAYLOR & FRANCIS LTD
DOI: 10.1080/10256016.2015.1016021
Keywords
Panama; evaporation; tropical hydrometeorology; hydrogen-2; oxygen-18; isotope hydrology; precipitation; ocean; meteoric water line; isotope fractionation
Funding
- Lendulet programme of the Hungarian Academy of Sciences [LP2012-27/2012]
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As calculated from data archived in the IAEA-WMO Global Network of Isotopes in Precipitation programme, the amount-weighted local meteoric water line for the Pacific coast of central Panama is: delta H-2 = 7.63(+/- 0.08) x delta O-18 + 6.51(+/- 0.49). Amount-weighted mean isotopic values were regressed against the sea surface temperature (SST) fields of the adjacent tropical oceans. A negative correlation of precipitation isotope composition with Caribbean SSTs is observed only for the early wet season (May-June), whilst the mid-summer dry period is characterized by positive correlation with eastern Pacific SSTs, similar to the late wet season (October-November). The negative response of May-June rainfall isotopic composition to Caribbean SSTs is explained by a SST-mediated change in stratiform rain fraction from organized convective systems proximal to the Inter Tropical Convergence Zone (ITCZ). The positive correlation for the rest of the wet season, when the organized convective zone of ITCZ and its attached stratiform belt are distant from the Pacific coast of Panama, is interpreted as simple evaporative temperature effect on isotopic fractionation.
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