Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Torbjörn E. Tornqvist"'
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-10 (2024)
Abstract Predicting climate impacts is challenging and has to date relied on indirect methods, notably modeling. Here we examine coastal ecosystem change during 13 years of unusually rapid, albeit likely temporary, sea-level rise ( > 10 mm yr−1) in
Externí odkaz:
https://doaj.org/article/7d3b6951f99d40859b3429e016745ed8
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Torbjörn E. Törnqvist, Michael D. Blum
Publikováno v:
Cambridge Prisms: Coastal Futures, Vol 2 (2024)
Major technological advances have made measurements of coastal subsidence more sophisticated, but these advances have not always been matched by a thorough examination of what is actually being measured. Here we draw attention to the widespread confu
Externí odkaz:
https://doaj.org/article/39260b7d0f414d37b77cd4908f0423e5
Autor:
Sönke Dangendorf, Noah Hendricks, Qiang Sun, John Klinck, Tal Ezer, Thomas Frederikse, Francisco M. Calafat, Thomas Wahl, Torbjörn E. Törnqvist
Publikováno v:
Nature Communications, Vol 14, Iss 1, Pp 1-11 (2023)
Abstract While there is evidence for an acceleration in global mean sea level (MSL) since the 1960s, its detection at local levels has been hampered by the considerable influence of natural variability on the rate of MSL change. Here we report a MSL
Externí odkaz:
https://doaj.org/article/3208791f3c6043979125cb055fc75a22
Publikováno v:
AGU Advances, Vol 2, Iss 1, Pp n/a-n/a (2021)
Abstract Floodplains of large alluvial rivers modulate the composition of riverine organic carbon (OC) and control OC oxidative loss, constituting a critical component in the global river‐atmosphere‐ocean carbon cycle. Therefore, anthropogenic ma
Externí odkaz:
https://doaj.org/article/ca149919460140568373480f99db7c06
Publikováno v:
AGU Advances, Vol 2, Iss 1, Pp n/a-n/a (2021)
Abstract Recent studies have produced conflicting results as to whether coastal wetlands can keep up with present‐day and future sea‐level rise. The stratigraphic record shows that threshold rates for coastal wetland submergence or retreat are lo
Externí odkaz:
https://doaj.org/article/6fc6599ede034d09b1f75495d011e8ff