AVANCES EN EL MONITOREO DEL GROSOR DEL HIELO MARINO Y NIEVE, DE LA DINAMICA OCEANICA Y CONTENIDO DE AGUA DULCE EN EL ARTICO USANDO DATOS DE TELEDETECCION
PID2021-125324OB-I00
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Nombre agencia financiadora Agencia Estatal de Investigación
Acrónimo agencia financiadora AEI
Programa Programa Estatal para Impulsar la Investigación Científico-Técnica y su Transferencia
Subprograma Subprograma Estatal de Generación de Conocimiento
Convocatoria Proyectos de I+D+i (Generación de Conocimiento y Retos Investigación)
Año convocatoria 2021
Unidad de gestión Plan Estatal de Investigación Científica y Técnica y de Innovación 2021-2023
Centro beneficiario AGENCIA ESTATAL CONSEJO SUPERIOR DE INVESTIGACIONES CIENTIFICAS (CSIC)
Identificador persistente http://dx.doi.org/10.13039/501100011033
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Resultados totales (Incluyendo duplicados): 1Encontrada(s) 1 página(s)
Contribución de congreso (ConferenceOutput). 2024
Sea Ice Meltwater in the Beaufort Gyre: A Comprehensive Analysis Using Sea Surface Salinity Data from SMOS
DIGITAL.CSIC. Repositorio Institucional del CSIC
- Andrés Marruedo, Eva de
- Umbert, Marta
- Sánchez Urrea, María
- González Gambau, Verónica
- Olmedo, Estrella
- Gabarró, Carolina
X Simposio de Estudios Polares, 15-17 May 2024, Salamanca.-- This work represents a contribution to the CSIC Thematic Interdisciplinary Platform PTI-POLARCSIC, Arctic sea ice is retreating, thinning, and exhibiting increased mobility. In the Beaufort Gyre (BG), liquid freshwater content has increased by 40% in the last two decades, with sea ice melting being a primary contributor. This study utilizes satellite observations of sea surface salinity (SSS) and sea ice concentration, along with model-based sea ice thickness from 2011 to 2019. The aim is to investigate the sea ice-SSS relationship at different scales in the Arctic and understand the sea-ice meltwater dynamics in the BG. Our findings reveal a strong synchrony and positive correlation between sea ice area and SSS in the Arctic Ocean. In September, when the BG exhibits the largest ice-free ocean surface, a noticeable release of freshwater from sea ice melting occurs, a phenomenon not accurately reproduced by the models. The SMOS (Soil Moisture and Ocean Salinity) mission proves valuable in detecting meltwater lenses (MWL) originating from sea ice melting. These MWLs exhibit mean SSS ranging from 19 psu at the begining of sea ice retreat to 25 psu before sea ice formation. Wind-driven anticyclonic eddies can trap MWLs, preserving the freshest SSS imprints on the sea surface for up to 10 days. Furthermore, events of sea surface salinification following sea ice formation suggest that SMOS SSS might be capturing information on brine rejection. The daily evolution of sea ice SSS within the MWLs demonstrates a tight correlation between both variables after sea ice melting and just before sea ice formation, indicating a transient period in between, E. De Andrés is supported by Margarita-Salas Grant No. UP2021-035 under the Next Generation-EU program. M. Umbert is funded by Marie Sk lodowska-Curie Grant Agreement No. 840374. This study was also financed by the MCIN/AEI projects DINGLAC (PID2020-113051RB-C31) and ARCTIC-MON (PID2021-125324OB-I00), and from the ESA Arctic+Salinity project (AO/1-9158/18/I-BG), Peer reviewed