Summary
A key dispute in palaeoclimate research is whether or not a permanent El Niño-like state, with warm waters spreading across the equatorial Pacific, existed during the late Miocene. Late Miocene climate was similar to the 4°C warming predicted for 2100 by the IPCC. As today’s El Niño causes global climate anomalies, a permanent El Niño-like state in the past may have had serious, global consequences, such as widespread aridity. MIONIÑO will test the existence of a late Miocene permanent El Niño-like state using geochemical microfossil records from recently recovered Western Pacific Warm Pool (WPWP) sediments and earth system modelling to assess equatorial Pacific conditions, their driving forces and global impacts.
MIONIÑO is timely, only being possible since the recovery of crucial WPWP samples in late 2016. MIONIÑO is also original and novel, presenting a new template for solving complicated climate questions using a new, robust stratigraphy and an interdisciplinary approach. UCL Earth Sciences is the ideal location to pursue state-of-the-art research in palaeoceanography and stratigraphy. Combining my existing expertise with key specialist knowledge from UCL researchers will equip me with the required skills to successfully complete MIONIÑO. I can hone my research vision and gain transferable skills to help me achieve my ultimate career goal of an academic research position.
MIONIÑO will advance past and future climate change research. Resolving the debate on permanent El Niño-like conditions in the late Miocene will discern whether warm El Niño events, as occurred in 2015/2016, become more frequent or evolve into a new mean state. Assessing causal links between permanent El Niño-like conditions and increased continental aridity will improve the future climate models that underpin European climate mitigation and adaptation strategies. MIONIÑO can further help us understand the true societal impact of more frequent or even permanent El Niño-like conditions.
MIONIÑO is timely, only being possible since the recovery of crucial WPWP samples in late 2016. MIONIÑO is also original and novel, presenting a new template for solving complicated climate questions using a new, robust stratigraphy and an interdisciplinary approach. UCL Earth Sciences is the ideal location to pursue state-of-the-art research in palaeoceanography and stratigraphy. Combining my existing expertise with key specialist knowledge from UCL researchers will equip me with the required skills to successfully complete MIONIÑO. I can hone my research vision and gain transferable skills to help me achieve my ultimate career goal of an academic research position.
MIONIÑO will advance past and future climate change research. Resolving the debate on permanent El Niño-like conditions in the late Miocene will discern whether warm El Niño events, as occurred in 2015/2016, become more frequent or evolve into a new mean state. Assessing causal links between permanent El Niño-like conditions and increased continental aridity will improve the future climate models that underpin European climate mitigation and adaptation strategies. MIONIÑO can further help us understand the true societal impact of more frequent or even permanent El Niño-like conditions.
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More information & hyperlinks
| Web resources: | https://cordis.europa.eu/project/id/796220 |
| Start date: | 23-04-2019 |
| End date: | 30-09-2022 |
| Total budget - Public funding: | 183 454,80 Euro - 183 454,00 Euro |
Cordis data
Original description
A key dispute in palaeoclimate research is whether or not a permanent El Niño-like state, with warm waters spreading across the equatorial Pacific, existed during the late Miocene. Late Miocene climate was similar to the 4°C warming predicted for 2100 by the IPCC. As today’s El Niño causes global climate anomalies, a permanent El Niño-like state in the past may have had serious, global consequences, such as widespread aridity. MIONIÑO will test the existence of a late Miocene permanent El Niño-like state using geochemical microfossil records from recently recovered Western Pacific Warm Pool (WPWP) sediments and earth system modelling to assess equatorial Pacific conditions, their driving forces and global impacts.MIONIÑO is timely, only being possible since the recovery of crucial WPWP samples in late 2016. MIONIÑO is also original and novel, presenting a new template for solving complicated climate questions using a new, robust stratigraphy and an interdisciplinary approach. UCL Earth Sciences is the ideal location to pursue state-of-the-art research in palaeoceanography and stratigraphy. Combining my existing expertise with key specialist knowledge from UCL researchers will equip me with the required skills to successfully complete MIONIÑO. I can hone my research vision and gain transferable skills to help me achieve my ultimate career goal of an academic research position.
MIONIÑO will advance past and future climate change research. Resolving the debate on permanent El Niño-like conditions in the late Miocene will discern whether warm El Niño events, as occurred in 2015/2016, become more frequent or evolve into a new mean state. Assessing causal links between permanent El Niño-like conditions and increased continental aridity will improve the future climate models that underpin European climate mitigation and adaptation strategies. MIONIÑO can further help us understand the true societal impact of more frequent or even permanent El Niño-like conditions.
Status
CLOSEDCall topic
MSCA-IF-2017Update Date
28-04-2024
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