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Project
This project investigates the effect of ocean mixing on biogeochemistry. We do so by combining different observational datasets, theoretical models, and mixing parameterizations to understand the ocean biological carbon pump.
The biological carbon pump influences how much carbon can be stored in the ocean, thereby directly influencing climate change. The temporal and spatial efficiency of the carbon pump is known to depend strongly on mixing, but exactly how remains unclear. Without an improved understanding of this coupling between ocean physics and biogeochemistry, there is little hope to really understand the global carbon cycle.
The PhD-student will work with the Mixation-I data. This includes physical data from four moorings deployed in the subtropical North Atlantic near Bermuda in April 2022. These moorings will be recovered in spring 2023. The Mixation-I data will be combined with physical and biogeochemical data from the Bermuda Atlantic Time-series Study, which comprises of monthly data from 1988 to present day. Additional datasets obtained through international collaborations will provide a unique opportunity to investigate the role of mixing on the biological carbon pump in different physical and biogeochemical regimes worldwide. We will combine these data with current mixing parametrizations and theoretical modeling of biogeochemical tracer dynamics to quantify the role of mixing in setting the ocean biological carbon pump.
Vacancy
The PhD-project is at the interface between ocean physics and biogeochemistry and combines both observational data with theoretical models. We encourage the student to participate in expeditions aboard research vessels, including the expedition to recover the Mixation-I moorings during spring 2023. The PhD candidate will be based at OCS (Texel), but will benefit from collaboration with international co-supervisors and collaborators.
The PhD-candidate we are looking for, should have a MSc. degree in a natural science such as – but not limited to – physical oceanography, fluid dynamics or applied mathematics. Preferably, you will also have:
We strive to ensure that our staff reflect the diversity of society, including age, gender and cultural background. We therefore very much appreciate candidates who are able to increase the diversity of NIOZ.
Employment of this full time position at Royal NIOZ is by NWO-I (The Netherlands Organization of Scientific Research). After a 12-month probationary period and successful evaluation, the position is extended for 36 months for a maximum employment of 4 years. The salary is compliant to the CAO-OI (Collective Labour Agreement for Dutch Research Institutes), a pension scheme, a holiday allowance of 8% of the gross annual salary, a year-end bonus of 8,3%, flexible work arrangements and arrangements and 42 days of holiday leave (fulltime position). You may expect attractive secondary employment conditions. We offer generous relocation expenses for employees coming from abroad and support with finding accommodation.
Royal NIOZ is located on the beautiful island of Texel in the World Heritage Wadden Sea. Texel offers sun, wind and beach, and a diverse but moderate level of facilities, including a thriving tourist industry, shops, sports facilities, primary schools and a high school. It is connected to the main land by an hourly to half-hourly ferry service, with crossings taking 20 minutes. The Royal NIOZ is situated next to the ferry terminal.
Researchers in the Department of Ocean System Research (OCS) study open-ocean processes from a variety of disciplines including physical and chemical oceanography, marine geology, paleoceanography and deep-sea ecology. We investigate the past and present ocean in order to assess its future role in the Earth system. We collect data during oceanographic research cruises and conduct experiments both at sea and in the laboratory at our home base on Texel. The department carries out work in diverse environments all around the globe, from the Antarctic to the Arctic, and from the Caribbean to the North Sea.
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