We present an investigation of the performance of the ECMWF coupled atmosphere-waves-ocean model for different ocean and atmosphere resolutions and coupling strategies on a series of tropical cyclones in the west Pacific with the aim to better understand the coupled feedback mechanisms in these extreme conditions.
For some of the test cases, we only find little impact of coupling the atmosphere to the ocean, while in others, we observe a very large impact. To further understand these differences, we have selected two tropical cyclones as case studies: TC Haiyan (with small impact of coupling) and TC Neoguri (with large impact of coupling). The comparison between these two cases suggests that the upper ocean stratification is the key to determine the strength of the coupled feedback. A strong coupled feedback is found whenever the ocean heat content of the upper layer is low while a very weak coupled feedback is found whenever the ocean has a thick warm mixed layer.
The oceanographic response to tropical cyclones has been compared for the two cases to surface information in the form of sea surface temperature and derived surface currents from drifting buoys and to subsurface observations from Argo and ship launched XBT’s. These comparisons show that we are able to realistically reproduce the atmospheric and oceanographic interaction during tropical cyclone conditions which gives us confidence that the coupled modelling system is physically sound.
BT - ECMWF Technical Memoranda DA - 2017 DO - 10.21957/dha6hjg4f LA - eng M1 - 794 N2 -
We present an investigation of the performance of the ECMWF coupled atmosphere-waves-ocean model for different ocean and atmosphere resolutions and coupling strategies on a series of tropical cyclones in the west Pacific with the aim to better understand the coupled feedback mechanisms in these extreme conditions.
For some of the test cases, we only find little impact of coupling the atmosphere to the ocean, while in others, we observe a very large impact. To further understand these differences, we have selected two tropical cyclones as case studies: TC Haiyan (with small impact of coupling) and TC Neoguri (with large impact of coupling). The comparison between these two cases suggests that the upper ocean stratification is the key to determine the strength of the coupled feedback. A strong coupled feedback is found whenever the ocean heat content of the upper layer is low while a very weak coupled feedback is found whenever the ocean has a thick warm mixed layer.
The oceanographic response to tropical cyclones has been compared for the two cases to surface information in the form of sea surface temperature and derived surface currents from drifting buoys and to subsurface observations from Argo and ship launched XBT’s. These comparisons show that we are able to realistically reproduce the atmospheric and oceanographic interaction during tropical cyclone conditions which gives us confidence that the coupled modelling system is physically sound.
PB - ECMWF PY - 2017 T2 - ECMWF Technical Memoranda TI - Tropical Cyclone Sensitivity to Ocean Coupling UR - https://www.ecmwf.int/node/16980 ER -