To evaluate the impact of the cellular response to warming oceans on the global biogeochemical cycles, we will use two computational models: The Cell Flux Model of Phytoplankton (CFM-Phyto) and MIT’s General Circulation Model (MIT-gcm). To run MIT-gcm, we require access to a high performance computing system. The main objectives of the project are to 1) Include CFM-Phyto in MIT-gcm’s representation of phytoplankton 2) Run various temperature scenarios 3) Evaluate/quantify the impact of the cell’s response to warming on global ocean cycles. These simulations will allow us to analyze the emerging elemental stoichiometry of phytoplankton in the surface ocean using data visualizations on maps of the global ocean. Additionally, these simulations may be used to illustrate the vertical distribution of carbon, which predict the differences in carbon export to the deep oceans depending on the effect of temperature, which has a great impact on climate regulation and long-term carbon storage.
The student will help get MIT-gcm running on the URI UNITY cluster and develop the optimal performance configuration to enable the multitude of simulations necessary for the overall goals of this research project.
Impact on oceanography: better representing lower trophic organisms in large ocean models. These organisms have a profound impact on ocean cycles and are often misrepresented. This model is a step towards making their physiology more realistic and represented in ocean models.
Impact to other disciplines: could lead to better climate predictions if applied to various models.
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Impact to society is a step toward a better climate model, which can be used for managing environments, such as fisheries.
Lessons learned: I learned to work on the HPC environment. I had zero experience and by the end of the project was able to modify and run an ocean model, which is rather complex on the HPC.
Overall results: changing ocean temperatures increases dedication of carbon to storage in lower trophic organisms, which may impact the nutritional quality of phytoplankton for higher trophic levels.