H2020Индивидуална стипендия2018–2021

CAP-ICE · CArbon Production of under-ICE phytoplankton blooms in a changing Arctic Ocean

„Хоризонт 2020“ — Действия „Мария Склодовска-Кюри“

Период
2018-01-15 → 2021-01-14
Финансиране от ЕС
264 668 €
Участници
2
Схема
MSCA-IF-GF

Линиите свързват координатора с партньорите.

Накратко на български

Цветенето на фитопланктон под леда в Северния ледови океан и механизмите за неговия растеж са в центъра на анализа. Това помага за по-точното разбиране на въглеродния цикъл и влиянието му върху климата на Земята.

Този кратък обзор е генериран от изкуствен интелект

Кратко обяснение, генерирано от езиков модел по текста на CORDIS. Оригиналът е по-долу.

Резултати накратко

CArbon Production of under-ICE phytoplankton blooms in a changing Arctic Ocean

Over the last decades, sea-ice in the Arctic Ocean (AO) has undergone unprecedented changes, with drastic decline in its extent, thickness and duration. Modern climate models are unable to simulate these changes, leading to large uncertainties in Arctic and Global Change predictions. Sea-ice strongly attenuates solar radiation and it is generally thought that phytoplankton, which drives Arctic marine CO2 sequestration, only grow in open waters once sea-ice retreats in spring. However, the discovery of large under-ice phytoplankton blooms (UIBs) growing beneath sea-ice contradicts this paradigm. UIB productivity in ice-covered regions has been suggested to be ten-fold larger than presently modeled. By initiating an international network (USA, France, Canada, Germany, Norway), the CAP-ICE project will acquire knowledge on the occurrence of UIBs, the physical mechanisms that control their initiation and productivity, and will quantify how UIBs affect the Arctic carbon cycle and climate. CAP-ICE will equally combine observational, modeling and novel technology approaches. Multiple pan-Arctic expeditions will provide new field observations on the environmental conditions controlling UIBs. Since UIBs are invisible to ocean color satellite sensors, developing a novel model adapted to under-ice environments will allow quantifying the contribution of UIBs to the Arctic carbon cycle. Finally, the recent launch of autonomous robotic platforms (Bio-Argo floats) will support the first assessment of UIB primary production and carbon export in AO and the implementation of a Bio-Argo Arctic network. By the end of this fellowship, CAP-ICE has made substantial contributions to the understanding of under-ice biogeochemical cycles through a combination of approaches. CAP-ICE has helped to provide the scientific community with needed knowledge and future directions for Arctic science. In addition, CAP-ICE has revealed new discoveries, not only in the Arctic, through the expansion of modern autonomous platforms. We are just at the beginning of a new era of rapid deployment of new autonomous systems in the Arctic, and CAP-ICE has contributed to this international effort.

Текст от CORDIS, на английски · Данни: CORDIS, © Европейски съюз

Цел на проекта

Over the last decades, sea-ice in the Arctic Ocean (AO) has undergone unprecedented changes, with drastic decline in its extent, thickness and duration. Modern climate models are unable to simulate these changes, leading to large uncertainties in Arctic and Global Change predictions. Sea-ice strongly attenuates solar radiation and it is generally thought that phytoplankton, which drives Arctic marine CO2 sequestration, only grow in open waters once sea-ice retreats in spring. However, the discovery of large under-ice phytoplankton blooms (UIBs) growing beneath sea-ice contradicts this paradigm. UIB productivity in ice-covered regions has been suggested to be ten-fold larger than presently modeled. By initiating an international network (USA, France, Canada, Germany, Norway), the CAP-ICE project will acquire knowledge on the occurrence of UIBs, the physical mechanisms that control their initiation and productivity, and will quantify how UIBs affect the Arctic carbon cycle and climate.CAP-ICE will equally combine observational, modeling and novel technology approaches. Multiple pan-Arctic expeditions will provide new field observations on the environmental conditions controlling UIBs. Since UIBs are invisible to ocean color satellite sensors, developing a novel model adapted to under-ice environments will allow quantifying the contribution of UIBs to the Arctic carbon cycle. Finally, the recent launch of autonomous robotic platforms (Bio-Argo floats) will support the first assessment of UIB primary production and carbon export in AO and the implementation of a Bio-Argo Arctic network. These inter-disciplinary and innovative activities will establish a two-way exchange of knowledge between the researcher/fellow and the host institutions and enhance their European and international competitiveness. Outcomes of CAP-ICE will have an impact on the European strategy for global ocean observations, enhance European research excellence, and address a major societal challenge.

Оригинален текст от CORDIS (на английски).

Участници

Връзки

Данни: CORDIS, © Европейски съюз