• Aucun résultat trouvé

Tropical extra-tropical thermocline water mass exchanges in the Community Climate Model v.3 Part I: the Atlantic Ocean

N/A
N/A
Info
Télécharger
Protected

Academic year: 2021

Partager "Tropical extra-tropical thermocline water mass exchanges in the Community Climate Model v.3 Part I: the Atlantic Ocean"

Copied!
11
0
0

Chargement.... (Voir le texte intégral maintenant)

Texte intégral

Figure

Fig. 1. Mean meridional versus vertical velocity (x1e 3 ) circulation vectors superimposed on the zonal velocity field (contour interval is 5 cm/s for T85 and T42 – upper panels – and 10 cm/s for POP3 – bottom panel)
Fig. 2. Climatological mean temperature ( ◦ C) at 30 ◦ W down to 300 m between 30 ◦ S–30 ◦ N for the (a) Levitus et al
Fig. 4. Climatological mean wind stress (vectors) and curl (shaded contours with interval of 0.5*0.1 N/m 2 ) for the coupled runs T85 and T42 (a) and (b), respectively, and (c) POP3-NCEP, which is the forcing for the ocean component
Fig. 5. Climatological mean absolute potential vorticity contours (c.i.=10 −10 m −1 s −1 ) and Salinity in grams/kilogram projected onto the isopycnal surface that crosses EUC core as a function of longitude and latitude for (a) POP3 at σ θ =25.3 (b) T85 a
+4

Références

Télécharger maintenant ( PDF - 11 Page - 3.66 MB )

Documents relatifs

Ocean Circulation Drives the Variability of the Carbon System in the Eastern Tropical Atlantic

The equatorial upwelling is also a productive region with a main phytoplankton bloom in July–August, when the Atlantic cold tongue is most developed, and a secondary

The Tropical Atlantic Observing System

The tropical Atlantic observing system is motivated by goals to understand and better predict phenomena such as tropical Atlantic interannual to decadal variability and climate

Mesoscale and seasonal variability of community production and respiration in the surface waters of the N.E. Atlantic Ocean

SST: Sea-surface temperature; MLD: mixed layer depth; ELD: euphotic layer depth; Tchl a: total chlorophyll a; TOC: total organic carbon; GCP: gross communityproduction; DCR:

The NOW regional coupled model: Application to the tropical Indian Ocean climate and tropical cyclone activity

Zhou (2011), Development and evaluation of a regional ocean-atmosphere coupled model with focus on the western North Pacific summer monsoon simulation: Impacts of different

A model perspective on the dynamics of the shadow zone of the eastern tropical North Atlantic – Part 1: the poleward slope currents along West Africa

In this context and pending further progress with model sensitivity experiments we hypothesize that mean poleward transport in the vicinity of the WA continental slope arises from

Nutrients and carbon fluxes in the estuaries of major rivers flowing into the tropical Atlantic

The concentrations of sil- icate in the three largest river estuaries (Amazon, Congo and Orinoco) were similar to those measured in the smaller river systems (Niger, São

Contribution of the Amazon River Discharge to Regional Sea Level in the Tropical Atlantic Ocean

This study uses a set of regional simulations based on the ocean model NEMO to quantify the influence of the Amazon runoff on sea level in the Tropical Atlantic Ocean.. The model

Some Observations on the 1955-1958 Excavations in the Cachette Court of Karnak

ةيبرعلا تاصخللما v inCEnT r ondoT 88CL681+94CL331 بيبل خيشلا - يتحب اعـل ةدابع شقن تولم-لولأا-مهسلا-ةوقلا-ديدشلا لىإ ًانابرق مدقي وهو سوسينويد سوين شرع