Adding Hernández-Lasheras paper

Author: erikvansebille

src/data/papers-citing-parcels.ts

@@ -2287,4 +2287,14 @@ export const papersCitingParcels: Paper[] = [
     abstract:
       'Sub-Antarctic Mode Waters (SAMWs) form to the north of the Antarctic Circumpolar Current in the Indo-Pacific Ocean, whence they ventilate the oceans lower pycnocline and play an important role in the climate system. With a backward Lagrangian particle-tracking experiment in a data-assimilative model of the Southern Ocean (B-SOSE), we address the long-standing question of the extent to which SAMWs originate from densification of southward-flowing subtropical waters versus lightening of northward-flowing Antarctic waters sourced by Circumpolar Deep Water (CDW) upwelling. Our analysis evidences the co-occurrence of both sources in all SAMW formation areas, and strong inter-basin contrasts in their relative contributions. Subtropical waters are the main precursor of Indian Ocean SAMWs (70%–75% of particles) but contribute a smaller amount (40% of particles) to Pacific SAMWs, which are mainly sourced from the upwelled CDW. By tracking property changes along particle trajectories, we show that SAMW formation from northern and southern sources involves contrasting drivers: subtropical source waters are cooled and densified by surface heat fluxes, and freshened by ocean mixing. Southern source waters are warmed and lightened by surface heat and freshwater fluxes, and they are made either saltier by mixing in the case of Indian SAMWs, or fresher by surface fluxes in the case of Pacific SAMWs. Our results underscore the distinct climatic impact of Indian and Pacific SAMWs formation, involving net release of atmospheric heat and uptake of atmospheric freshwater, respectively; a role that is conferred by the relative contributions of subtropical and Antarctic sources to their formation.',
   },
+  {
+    title:
+      'High frequency radar observing system simulation experiment in the Western Mediterranean Sea. A Lagrangian assessment approach',
+    published_info: 'Ocean Modelling, in press',
+    authors:
+      'Hernández-Lasheras, J, A Orfila, A Santana, I Hernandez-Carrasco, B Mourre (2025)',
+    doi: 'https://doi.org/10.1016/j.ocemod.2025.102553',
+    abstract:
+      'The potential impact of the inclusion of new antenas in a HFR system is evaluated through an Observing System Simulation Experiment (OSSE) in the Ibiza Channel (Western Mediterranean Sea). Two different configurations of the same model are used: i) a Nature Run considered as the real ocean state, is used to generate pseudo-observations, and ii) a Control Run , where the pseudo-observations are assimilated. The OSSE is first validated by comparison against a previous Observing System Experiment (OSE). The impact of the new antennas for forecasting surface currents is evaluated in two different periods with different levels of agreement between NR and CR. The HFR expansion is found to contribute to significantly correct the circulation patterns in the Channel, leading to surface meridional velocity error reductions up to 19%. The improvement on surface transport in the area is analyzed in the Lagrangian framework, taking advantage of the full ocean state knowledge given by the OSSE. Results show that DA can help to better represent the Lagrangian Coherent Structures present in the NR.',
+  },
 ]