d18O (WEB1fa7c61b): paleoData_longName: '' has been replaced by 'AD'
year (WEBbdfce92d): paleoData_units: 'AD' has been replaced by 'yr AD'
year (WEBbdfce92d): paleoData_longName: '' has been replaced by 'AD'

Brienen, R. J. W., Helle, G., Pons, T. L., Guyot, J.-L. and Gloor, M.: Oxygen isotopes in tree rings are a good proxy for Amazon precipitation and El Nino-Southern Oscillation variability, Proceedings of the National Academy of Sciences, 109(42), 16957–16962, doi:10.1073/pnas.1205977109, 2012.

Oxygen isotopes in tree rings are a good proxy for Amazon precipitation and El Nino-Southern Oscillation variability

Changed isotopeInterpretation1_name from 'Palmer Draought Severity Index(combined effect o f temperature and precipitation amount)' to standardized equivalent P_E - check direction (GF)

OCh-S: In 1 file has been presented 6 graphs, which were presented later on again. Either leave 1 file with 6 graphs, or present only 1 graph with own link. Label is desapeer 06, 01, 02, 03, 04, 05. Same graphs repeated 5 times with different links.

As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched d18O in tree rings?..moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor...Although the mechanisms underlying variations in tree ring d18O can generally be attributed to d18O of source water and evaporative enrichment of leaf water d18O, in pluvial monsoon regions these effects seem to be well represented by the PDSI,

As recorded in the meteorological data from the monsoon season, higher temperatures usually correlate with lower precipitation, and relative humidity levels, both of which lead to enriched 18O in tree rings. Moreover, as climate parameters are significantly correlated with one another, it is difficult to identify a dominant factor. Although the mechanisms underlying variations in tree- ring d18O can generally be attributed to d18O of source water and evaporative enrichment of 18O leaf water, in pluvial monsoon regions these effects seem to be well represented by the PDSI.