Wolfgang Koeve
Biographic Data
| ID | 7993965 |
|---|---|
| NAME | Wolfgang Koeve |
| GIVEN NAMES | Wolfgang |
| FAMILY NAME | Koeve |
| SIGNATURE | KOEVE W |
| AFFILIATIONS | GEOMAR Helmholtz Centre for Ocean Research Kiel |
| ORCID | 0000-0002-2298-9230 |
| VERIFIED | Yes |
| TOTAL WORKS | 4 |
| TOTAL CITATIONS | 0 |
| WORKS AS AUTHOR | 4 |
| WORKS AS EDITOR | 0 |
| FIRST PUBLICATION YEAR | 2016 |
| LATEST PUBLICATION YEAR | 2025 |
| H-INDEX | 0 |
Direct cooling effect of artificial upwelling dominates over its marine carbon dioxide removal potential
Artificial upwelling (AU) is investigated as a marine carbon dioxide removal (CDR) method with a strong focus on its potential impact on Earth’s carbon cycle, in particular enhanced air-sea CO 2 flux. The overarching goal of marine CDR methods is to contribute to offsetting remaining CO 2 emissions as a means to stabilize global mean surface air temperature (SAT). However, AU also directly affects ocean heat uptake (OHU) through the upwelling of …
The response of the ocean carbon cycle to artificial upwelling, ocean iron fertilization and the combination of both
Artificial upwelling (AU) and ocean iron fertilization (OIF) both have been proposed as marine carbon dioxide removal methods to enhance ocean carbon uptake by stimulating the biological carbon pump. We simulate global and regional AU and OIF individually and the combination of both methods between the years 2025 and 2100 in ocean-atmosphere model experiments under the moderate RCP 4.5 CO 2 -emission pathway and show that the combination of globa…
Hierarchy of calibrated global models reveals improved distributions and fluxes of biogeochemical tracers in models with explicit representation of iron
Iron is represented in biogeochemical ocean models by a variety of structurally different approaches employing generally poorly constrained empirical parameterizations. Increasing the structural complexity of iron modules also increases computational costs and introduces additional uncertainties, with as yet unclear benefits. In order to demonstrate the benefits of explicitly representing iron, we calibrate a hierarchy of iron modules and evaluat…
Could artificial ocean alkalinization protect tropical coral ecosystems from ocean acidification
Artificial ocean alkalinization (AOA) is investigated as a method to mitigate local ocean acidification and protect tropical coral ecosystems during a 21st century high CO 2 emission scenario. Employing an Earth system model of intermediate complexity, our implementation of AOA in the Great Barrier Reef, Caribbean Sea and South China Sea regions, shows that alkalinization has the potential to counteract expected 21st century local acidification i…
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Could artificial ocean alkalinization protect tropical coral ecosystems from ocean acidification
Artificial ocean alkalinization (AOA) is investigated as a method to mitigate local ocean acidification and protect tropical coral ecosystems during a 21st century high CO 2 emission scenario. Employing an Earth system model of intermediate complexity, our implementation of AOA in the Great Barrier Reef, Caribbean Sea and South China Sea regions, shows that alkalinization has the potential to counteract expected 21st century local acidification i…
Hierarchy of calibrated global models reveals improved distributions and fluxes of biogeochemical tracers in models with explicit representation of iron
Iron is represented in biogeochemical ocean models by a variety of structurally different approaches employing generally poorly constrained empirical parameterizations. Increasing the structural complexity of iron modules also increases computational costs and introduces additional uncertainties, with as yet unclear benefits. In order to demonstrate the benefits of explicitly representing iron, we calibrate a hierarchy of iron modules and evaluat…
The response of the ocean carbon cycle to artificial upwelling, ocean iron fertilization and the combination of both
Artificial upwelling (AU) and ocean iron fertilization (OIF) both have been proposed as marine carbon dioxide removal methods to enhance ocean carbon uptake by stimulating the biological carbon pump. We simulate global and regional AU and OIF individually and the combination of both methods between the years 2025 and 2100 in ocean-atmosphere model experiments under the moderate RCP 4.5 CO 2 -emission pathway and show that the combination of globa…
Direct cooling effect of artificial upwelling dominates over its marine carbon dioxide removal potential
Artificial upwelling (AU) is investigated as a marine carbon dioxide removal (CDR) method with a strong focus on its potential impact on Earth’s carbon cycle, in particular enhanced air-sea CO 2 flux. The overarching goal of marine CDR methods is to contribute to offsetting remaining CO 2 emissions as a means to stabilize global mean surface air temperature (SAT). However, AU also directly affects ocean heat uptake (OHU) through the upwelling of …
Chemistry (4 works) · Environmental Science (4 works) · Geology (3 works) · Ocean Acidification Effects and Responses (3 works) · Oceanography (3 works) · Biology (2 works) · Carbon dioxide (2 works) · Ecology (2 works) · Ecosystem (2 works) · Environmental Chemistry (2 works)