Dersleri yüzünden oldukça stresli bir ruh haline sikiş hikayeleri bürünüp özel matematik dersinden önce rahatlayabilmek için amatör pornolar kendisini yatak odasına kapatan genç adam telefonundan porno resimleri açtığı porno filmini keyifle seyir ederek yatağını mobil porno okşar ruh dinlendirici olduğunu iddia ettikleri özel sex resim bir masaj salonunda çalışan genç masör hem sağlık hem de huzur sikiş için gelip masaj yaptıracak olan kadını gördüğünde porn nutku tutulur tüm gün boyu seksi lezbiyenleri sikiş dikizleyerek onları en savunmasız anlarında fotoğraflayan azılı erkek lavaboya geçerek fotoğraflara bakıp koca yarağını keyifle okşamaya başlar
Reach Us +1-845-458-6882
GET THE APP
Seasonal And Interannual Variability Of The Surface Mixed Layer Heat Budget In The Caribbean Sea | 18489
ISSN: 2155-9910
Journal of Marine Science: Research & Development
Open Access
Like us on:
Our Group organises 3000+ Global Conferenceseries Events every year across USA, Europe & Asia with support from 1000 more scientific Societies and Publishes 700+ Open Access Journals which contains over 50000 eminent personalities, reputed scientists as editorial board members.
The seasonal and interannual variations of the mixed layer depth (MLD) and the heat stored within this layer inthe Caribbean
Sea have been investigated from temperature and salinity profiles obtained from the high resolution (daily; 0.25?lat/lon)
GLORYS-Mercator reanalysis model data for the 1992-2009 period.In this region the MLD is relatively shallow, oscillating
from 10 to 90 m depth during the annual cycle, with the maximum values observed during the dry season (December to
March). Spatially, the highest (lowest) depths were found in the northwestern (coastal region), in agreement with the wind
stress curl pattern which induces down welling (upwelling) of the Ekman layer, respectively. The MLD oscillations depend on
the intensity of the zonal winds and the location of the Caribbean Low Level Jet (CLLJ). The isothermal layer depth was found
to be deeper than the MLD. These differences in depth have been associated with the presence of sub-superficial temperature
inversions. The barrier layer depth can reach up to 60 m. Data show no significant differences of the MLD due to El Ni?o-
La Ni?a (ENSO) events, but rather a Quasi-Biennial Oscillation (QBO) is observed to influence this region at interannual
timescales. The seasonal ocean heat stored within the mixed layer oscillated between -285 y 240Wm
−2
. During the dry season
(rainy season), when the MLD is deep (shallow) the region loses (gains) heat. This is determined by air-water fluxes being the
net short wave radiation the main gain, and the latent heat the main loss at both timescales.
Biography
Raul A Montoya is an Oceanographer that has recently (April 2014) completed his Master degree in Engineering of Hydraulic Resources from the National
University of Colombia, in Medellin and this research is part of his thesis. He is now starting his PhD studies in the same educational institution and is part of
the OCEANICOS research group of Oceanography and Coastal Engineering. He has participated in several investigations and is co-author of many papers in
oceanography and renewable energy journals.
Relevant Topics
Peer Reviewed Journals
Make the best use of Scientific Research and information from our 700 + peer reviewed, Open Access Journals