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Eliades, M.; Bruggeman, A.; Djuma, H.; Christofi, C.; Kuells, C. |
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Quantifying evapotranspiration and drainage losses in a semi-arid nectarine (Prunus persica var. nucipersica) field with a dynamic crop coefficient (Kc) derived from leaf area index measurements |
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2022 |
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Water |
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14 |
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5 |
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734 |
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Mdpi |
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THL @ christoph.kuells @ eliades2022quantifying |
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211 |
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Mehraein, M.; Mohanavelu, A.; Naganna, S.R.; Kulls, C.; Kisi, O. |
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Monthly streamflow prediction by metaheuristic regression approaches considering satellite precipitation data |
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Journal Article |
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2022 |
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Water |
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14 |
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22 |
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3636 |
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THL @ christoph.kuells @ mehraein2022monthly |
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219 |
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Castrignanò, A.; Buttafuoco, G.; Giasi, C. |
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Assessment of groundwater salinisation risk using multivariate geostatistics |
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Book Chapter |
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2008 |
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geoENV VI – Geostatistics for Environmental Applications |
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15 |
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191-202 |
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Springer, Dordrecht |
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A., S.; M.J., P.; R., D. |
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CUT @ phaedon.kyriakidis @ Castrignano2008 |
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119 |
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Park, H.; Schlesinger, W. |
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Title |
Global biochemical cycle of boron |
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2002 |
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Global Biogeochemical Cycles |
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16 |
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1072 |
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The global Boron (B) cycle is primarily driven by a large flux (1.44 Tg B/yr) through the atmosphere derived from seasalt aerosols. Other significant sources of atmospheric boron include emissions during the combustion of biomass (0.26-0.43 Tg B/yr) and coal, which adds 0.20 Tg B/yr as an anthropogenic contribution. These known inputs to the atmosphere cannot account for the boron removed from the atmosphere during rainfall (3.0 Tg B/yr) and estimated dry deposition (1.3-2.7 Tg B/yr). In addition to atmospheric deposition, rock weathering is a source of boron (0.19 Tg B/yr) for terrestrial ecosystems, and humans mine about 0.31 Tg B/yr from the Earth's crust. More than 4.8 Tg B/yr circulates in the biogeochemical cycle of land plants, and about 0.53-0.63 Tg B/yr is carried from land to sea by rivers. The biogeochemical cycle of boron in the sea includes 4.4 Tg B/yr circulating in the marine biosphere, and an annual loss of 0.47 Tg B/yr to the oceanic crust via a variety of sedimentary processes that collectively remove only a small fraction of the total annual inputs to the oceans. Thus with our current understanding of the global biogeochemistry of B, the atmospheric budget shows outputs > inputs, while the marine compartments show inputs > outputs. Despite these uncertainties, it is clear that the human perturbation of the global B cycle has more than doubled the mobilization of B from the crust and contributes significantly to the B transport in rivers. |
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THL @ luqianxue.zhang @ article |
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94 |
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Li*, L.; Zhou, H.; Franssen, H.J.H.; Gómez-Hernández, J.J. |
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Groundwater flow inverse modeling in non-MultiGaussian media: performance assessment of the normal-score Ensemble Kalman Filter |
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2012 |
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Hydrol. Earth Syst. Sci. |
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16 |
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2 |
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573-590 |
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Copernicus GmbH |
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CUT @ phaedon.kyriakidis @ Li2012 |
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154 |
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