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  • 1
    Publication Date: 2015-10-29
    Description: Seasonal information of temperature, salinity, dissolved oxygen (DO) and chlorophyll, combined with meteorological and river discharge time series were used to describe the oceanographic conditions in the Reloncavi fjord (41°35' S; 72°20' W). The winds in the fjord valley blow mainly down-fjord during winter, reinforcing the upper layer outflow, while in spring–summer winds have a predominant up-fjord direction contrary to upper layer outflow. The fjord, with a deep sill at the mouth, was well stratified year-round and showed a thin surface layer of brackish water with mean salinities between 10.4 ± 1.4 (spring) and 13.2 ± 2.5 (autumn). The depth of the upper layer changed slightly along the different studied seasons remaining at about 4.5 m near the mouth. This upper layer presented a mean outflow (Q1) of 3185 ± 223 m3 s−1, which imply a flushing time of about 3 days of this layer. The vertical salt flux was ∼ 37 tons of salt per second, similar to the horizontal salt flux observed in the upper layer. These estimations will contribute to a better management of the aquaculture on this region.
    Print ISSN: 1812-0806
    Electronic ISSN: 1812-0822
    Topics: Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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  • 2
    Publication Date: 2015-07-30
    Description: This research reveals new insights into the climatic drivers of anomalies in land surface phenology (LSP) across the entire European forest, while at the same time establishes a new conceptual framework for predictive modelling of LSP. Specifically, the Random Forest method, a multivariate, spatially non-stationary and non-linear machine learning approach, was introduced for phenological modelling across very large areas and across multiple years simultaneously: the typical case for satellite-observed LSP. The RF model was fitted to the relation between LSP anomalies and numerous climate predictor variables computed at biologically-relevant rather than human-imposed temporal scales. In addition, the legacy effect of an advanced or delayed spring on autumn phenology was explored. The RF models explained 81 and 62 % of the variance in the spring and autumn LSP anomalies, with relative errors of 10 and 20 %, respectively: a level of precision that has until now been unobtainable at the continental scale. Multivariate linear regression models explained only 36 and 25 %, respectively. It also allowed identification of the main drivers of the anomalies in LSP through its estimation of variable importance. This research, thus, shows clearly the inadequacy of the hitherto applied linear regression approaches for modelling LSP and paves the way for a new set of scientific investigations based on machine learning methods.
    Print ISSN: 1810-6277
    Electronic ISSN: 1810-6285
    Topics: Biology , Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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