In temperate European climates, soil water removal due to vegetation transpiration peaks in summer and soil rewetting from higher levels of precipitation occurs in winter. In clays of high plasticity, the seasonal cycles of drying and wetting cause the soil to experience a volumetric change, resulting in seasonal shrinking and swelling. For a clay slope exhibiting volume change, such behaviour ...

Observations near a large tabular iceberg in theWeddell Sea inMarch and April 2009 show evidence that water from ice melting below the surface is dispersed in two distinct ways. Warm, salty anomalies in T–S diagrams suggest that water from the permanent thermocline is transported vertically as a result of turbulent entrainment of meltwater at the iceberg’s base. Stepped profiles of temperature,...

Sinking organic particles from surface waters provide key nutrients to the deep ocean, and could serve as vectors transporting microbial diversity ocean. However, effect of this seasonally varying connectivity with on communities remains unexplored. Here, a three-year time-series (500 m) part Munida Microbial Observatory Time-Series (MOTS) was used study seasonality epipelagic mesopelagic proka...

This study assessed seasonal and regional trends of pharmaceuticals and personal care products (PPCPs) detected in monthly samples from two local wastewater treatment plants (WWTPs) in Charleston, South Carolina, USA, over the period of one year. Surface water of Charleston Harbor was also analyzed to examine environmental distribution in an estuarine ecosystem. Of the 19 compounds examined, 11...

[1] Time-series datasets of surface-water biogenic silica (bSiO2) and deep-water bSiO2 export in the Santa Barbara Channel (SBC) allow for elucidation of the important scales of spatial and temporal variability and an evaluation of potential controlling mechanisms. Changes in local upwelling strength is the most important factor controlling seasonal variations for the surface bSiO2 dataset and ...

BACKGROUND Seasonal changes in pore water and sediment redox geochemistry have been observed in many near-surface sediments. Such changes have the potential to strongly influence trace metal distribution and thus create seasonal fluctuations in metal mobility and bioavailability. RESULTS Seasonal trends in pore water and sediment geochemistry are assessed in the upper 50 cm of littoral kettle...