Caroline Katsman
Biographic Data
| ID | 6817862 |
|---|---|
| NAME | Caroline Katsman |
| GIVEN NAMES | Caroline |
| FAMILY NAME | Katsman |
| SIGNATURE | KATSMAN C |
| AFFILIATIONS | Delft University of Technology |
| ORCID | 0000-0001-7297-0311 |
| VERIFIED | Yes |
| TOTAL WORKS | 2 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 2 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2014 |
| LATEST PUBLICATION YEAR | 2026 |
| H-INDEX | 0 |
Multi‐Stability of the Present‐Day Atlantic Meridional Overturning Circulation
The Atlantic Meridional Overturning Circulation (AMOC) plays a key role in the climate system, especially in the global meridional heat transport. Historical reconstructions indicate that the AMOC has weakened by about 15% since the mid‐20th century. Paleoclimate records, ocean theory, as well as a hierarchy of climate models suggest that the AMOC is a tipping element, sensitive to changes in buoyancy fluxes at the air‐sea interface, and could tr…
Constructing scenarios of regional sea level change using global temperature pathways
The effects of sea level change become increasingly relevant for the Dutch coast. Therefore we construct two scenarios for regional sea-level change in the 21st century. They are designed to follow two temperature pathways, in which global mean temperature rises moderately ('G', +1.5 K in 2085) or more substantially ('W', +3.5 K in 2085). Contributions from all major processes leading to sea level rise are included (ocean expansion, glacier melt,…
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Constructing scenarios of regional sea level change using global temperature pathways
The effects of sea level change become increasingly relevant for the Dutch coast. Therefore we construct two scenarios for regional sea-level change in the 21st century. They are designed to follow two temperature pathways, in which global mean temperature rises moderately ('G', +1.5 K in 2085) or more substantially ('W', +3.5 K in 2085). Contributions from all major processes leading to sea level rise are included (ocean expansion, glacier melt,…
Multi‐Stability of the Present‐Day Atlantic Meridional Overturning Circulation
The Atlantic Meridional Overturning Circulation (AMOC) plays a key role in the climate system, especially in the global meridional heat transport. Historical reconstructions indicate that the AMOC has weakened by about 15% since the mid‐20th century. Paleoclimate records, ocean theory, as well as a hierarchy of climate models suggest that the AMOC is a tipping element, sensitive to changes in buoyancy fluxes at the air‐sea interface, and could tr…
Climate change (2 works) · Climate model (2 works) · Climate variability and models (2 works) · Geology and Paleoclimatology Research (2 works) · Abrupt climate change (1 work) · Antarctic ice sheet (1 work) · Climate system (1 work) · Climatology (1 work) · Computer Science (1 work) · Cryosphere (1 work)