Name: | Description: | Size: | Format: | |
---|---|---|---|---|
333.89 KB | Adobe PDF |
Advisor(s)
Abstract(s)
As we retreat into historical time, the attempt to reconstruct past climates and their impact in
the ecosystems becomes increasingly complex. This study makes a correlation between solar
radiation and the growth of a sandy spit that allowed the formation of the Aveiro’s lagoon.
Knowing the controversy surrounding the use of a single proxy for the definition of phenomena as complex as climate fluctuations, whenever possible, a link is established between the
average rates of annual progression of the sandy spit with the known data of the NAO (North
Atlantic Oscillation) and the great climatic periods. A more intense pace of development is
found during the Medieval Warm Period, that is fallen to a speed of about half during the Little
Ice Age.
Description
Keywords
Climate Solar radiation North coast Portuguese Coastal morph dynamics
Citation
Publisher
Academia Letters