Such as wildfire feedback,
coastal erosion, weather / atmospheric anomalies,
seasonal changes, species adaptation, ocean currents etc..
•
Seasonal forecasting for water allocation and irrigated agriculture (IMPREX project) Johannes Hunink, Futurewater — presentation pdf • PEARL Project — preparing for extremes and rare event in
coastal regions — Uwe Mikolajewicz, MPI - MET — presentation pdf • Commercial climate services — lessons learned from the Klimaspring campaign — Mikkel A. Thomassen, Smith Innovation — presentation pdf • Climate
change impact on water resources — Experiences with different climates / scales / tools — Philipp Stanzel, Poyry Energy — presentation pdf • Climate
change effect study for the Frisian Belt canal water system - Peter Schaper, Wetterskipfryslan — presentation pdf
Changes in the watershed can, for example, lead to changes in alkalinity and CO2 fluxes that, together with metabolic processes and oceanic dynamics, yield high - magnitude decadal changes of up to 0.5 units in coastal pH. Metabolism results in strong diel to seasonal fluctuations in pH, with characteristic ranges of 0.3 pH units, with metabolically intense habitats exceeding this range on a daily
Changes in the watershed can, for example, lead to
changes in alkalinity and CO2 fluxes that, together with metabolic processes and oceanic dynamics, yield high - magnitude decadal changes of up to 0.5 units in coastal pH. Metabolism results in strong diel to seasonal fluctuations in pH, with characteristic ranges of 0.3 pH units, with metabolically intense habitats exceeding this range on a daily
changes in alkalinity and CO2 fluxes that, together with metabolic processes and oceanic dynamics, yield high - magnitude decadal
changes of up to 0.5 units in coastal pH. Metabolism results in strong diel to seasonal fluctuations in pH, with characteristic ranges of 0.3 pH units, with metabolically intense habitats exceeding this range on a daily
changes of up to 0.5 units in
coastal pH. Metabolism results in strong diel to
seasonal fluctuations in pH, with characteristic ranges of 0.3 pH units, with metabolically intense habitats exceeding this range on a daily basis.
In continental fluvial and
coastal sections,
changes in siliciclastic depositional facies reflect on increased frequency of high - energy events (e.g., extreme flooding), possibly from monsoon - like
seasonal rains, and / or from unusually intense and / or sustained extra-tropical storms.