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Author Misra, V.; Selman, C.; Waite, A. J.; Bastola, S.; Mishra, A. url  doi
openurl 
  Title Terrestrial and Ocean Climate of the 20th Century Type $loc['typeBook Chapter']
  Year 2017 Publication Florida's climate: Changes, variations, & impacts Abbreviated Journal  
  Volume Issue Pages 485-509  
  Keywords Seasonal cycle; Diurnal variations; Sea breeze; ENSO; Tropical cyclones; Hurricanes; AWP; AMO; PDO; PIZA  
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  Publisher Florida Climate Institute Place of Publication Gainesville, FL Editor Chassignet, E. P.; Jones, J. W.; Misra, V.; Obeysekera, J.  
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  Funding Approved $loc['no']  
  Call Number COAPS @ mfield @ Serial 849  
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Author Xu, X.; Chassignet, E.P., Wang, F. url  doi
openurl 
  Title On the variability of the Atlantic meridional overturning circulation transports in coupled CMIP5 simulations Type $loc['typeJournal Article']
  Year 2018 Publication Climate Dynamics Abbreviated Journal Clim Dyn.  
  Volume 51 Issue 11 Pages 6511-6531  
  Keywords NAO-AMOC; CMIP5; NAO index; AMOC index; meridional pressure gradient; magnitude; structure change of the NAO.  
  Abstract The Atlantic meridional overturning circulation (AMOC) plays a fundamental role in the climate system, and long-term climate simulations are used to understand the AMOC variability and to assess its impact. This study examines the basic characteristics of the AMOC variability in 44 CMIP5 (Phase 5 of the Coupled Model Inter-comparison Project) simulations, using the 18 atmospherically-forced CORE-II (Phase 2 of the Coordinated Ocean-ice Reference Experiment) simulations as a reference. The analysis shows that on interannual and decadal timescales, the AMOC variability in the CMIP5 exhibits a similar magnitude and meridional coherence as in the CORE-II simulations, indicating that the modeled atmospheric variability responsible for AMOC variability in the CMIP5 is in reasonable agreement with the CORE-II forcing. On multidecadal timescales, however, the AMOC variability is weaker by a factor of more than 2 and meridionally less coherent in the CMIP5 than in the CORE-II simulations. The CMIP5 simulations also exhibit a weaker long-term atmospheric variability in the North Atlantic Oscillation (NAO). However, one cannot fully attribute the weaker AMOC variability to the weaker variability in NAO because, unlike the CORE-II simulations, the CMIP5 simulations do not exhibit a robust NAO-AMOC linkage. While the variability of the wintertime heat flux and mixed layer depth in the western subpolar North Atlantic is strongly linked to the AMOC variability, the NAO variability is not.  
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  Call Number COAPS @ rl18 @ Serial 981  
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Author Bruno-Piverger, R.E. url  openurl
  Title Applying Neural Networks to Simulate Visual Inspection of Observational Weather Data Type $loc['typeJournal Article']
  Year 2019 Publication Florida State University College of Arts and Sciences, Master's Thesis Abbreviated Journal  
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  Call Number COAPS @ user @ Serial 1090  
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Author Sullivan, D; Murphree, T; Rosenfeld, L; Sullivan, D; Smith, S url  openurl
  Title Knowledge and Skill Guidelines for Marine Science and Technology: Operational Marine Forecasters Type $loc['typeMiscellaneous']
  Year 2011 Publication Marine Advanced Technology Education Center Abbreviated Journal  
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  Call Number COAPS @ mfield @ Serial 330  
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Author Stukel, M.R.; Biard, T.; Krause, J.W.; Ohman, M.D. url  doi
openurl 
  Title Large Phaeodaria in the twilight zone: Their role in the carbon cycle Type $loc['typeJournal Article']
  Year 2018 Publication Association for the Sciences of Limnology and Oceanography Abbreviated Journal  
  Volume Issue Pages  
  Keywords Carbon cycle; Ocean; Twilight zone, Rhizarian measurements; Aulosphaeridae  
  Abstract Advances in in situ imaging allow enumeration of abundant populations of large Rhizarians that compose a substantial proportion of total mesozooplankton biovolume. Using a quasi-Lagrangian sampling scheme, we quantified the abundance, vertical distributions, and sinking&#8208;related mortality of Aulosphaeridae, an abundant family of Phaeodaria in the California Current Ecosystem. Inter&#8208;cruise variability was high, with average concentrations at the depth of maximum abundance ranging from < 10 to > 300 cells m&#8722;3, with seasonal and interannual variability associated with temperature&#8208;preferences and regional shoaling of the 10°C isotherm. Vertical profiles showed that these organisms were consistently most abundant at 100&#65533;150&#8201;m depth. Average turnover times with respect to sinking were 4.7&#65533;10.9 d, equating to minimum in situ population growth rates of ~ 0.1&#65533;0.2 d&#8722;1. Using simultaneous measurements of sinking organic carbon, we find that these organisms could only meet their carbon demand if their carbon : volume ratio were ~ 1 &#956;g C mm&#8722;3. This value is substantially lower than previously used in global estimates of rhizarian biomass, but is reasonable for organisms that use large siliceous tests to inflate their cross&#8208;sectional area without a concomitant increase in biomass. We found that Aulosphaeridae alone can intercept > 20% of sinking particles produced in the euphotic zone before these particles reach a depth of 300&#8201;m. Our results suggest that the local (and likely global) carbon biomass of Aulosphaeridae, and probably the large Rhizaria overall, needs to be revised downwards, but that these organisms nevertheless play a major role in carbon flux attenuation in the twilight zone.  
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  Call Number COAPS @ user @ Serial 967  
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Author Hanley, DE; Jagtap, S; LaRow, TE; Jones, JW; Cocke, S; Zierden, D; O'Brien, JJ url  openurl
  Title The linkage of regional climate models to crop models Type $loc['typeConference Article']
  Year 2002 Publication 3rd Symposium on Environmental Applications Abbreviated Journal  
  Volume Issue Pages 134-139  
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  Area Expedition Conference 3rd Symposium on Environmental Applications  
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  Call Number COAPS @ mfield @ Serial 501  
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Author Subrahmanyam, B.; Manghanai, V.; O'Brien, J. J.; Morrison, J. M.; Xie, L. url  openurl
  Title A study of the Indian Ocean Dipole Mode Dynamics using satellite observations and MICOM simulations Type $loc['typeConference Article']
  Year 2001 Publication Abbreviated Journal  
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  Publisher Place of Publication San Diego, California, USA Editor  
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  Funding Approved $loc['no']  
  Call Number COAPS @ mfield @ Serial 823  
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Author Bourassa, M. A. url  openurl
  Title Tehuantepec wind and pressure changes associated with tropical cyclones Type $loc['typeConference Article']
  Year 2001 Publication 11th Conference on Interactions of the Sea and Atmosphere, Amer. Meteor. Soc., San Diego, CA, USA Abbreviated Journal  
  Volume Issue Pages 27-28  
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  Funding NASA, SEAWINDS, OVWST Approved $loc['no']  
  Call Number COAPS @ mfield @ Serial 815  
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Author Groenen, D.; Misra, V. url  openurl
  Title Characterization of the Rainy Season of Mesoamerica Type $loc['typeConference Article']
  Year 2016 Publication Abbreviated Journal  
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  Publisher American Meteorological Society Place of Publication Editor  
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  Area Expedition Conference 32nd Conference on Hurricanes and Tropical Meteorology  
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  Call Number COAPS @ mfield @ Serial 76  
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Author Wang, S.; Kranz, S.A.; Kelly, T.B.; Song, H.; Stukel, M.R.; Cassar, N. url  doi
openurl 
  Title Lagrangian Studies of Net Community Production: The Effect of Diel and Multiday Nonsteady State Factors and Vertical Fluxes on O2/Ar in a Dynamic Upwelling Region Type $loc['typeJournal Article']
  Year 2020 Publication Journal of Geophysical Research: Biogeosciences Abbreviated Journal J. Geophys. Res. Biogeosci.  
  Volume 125 Issue 6 Pages e2019JG005569  
  Keywords net community production; O2/Ar; California Current Ecosystem; Lagrangian measurements; vertical fluxes; nonsteady state  
  Abstract The ratio of dissolved oxygen to argon in seawater is frequently employed to estimate rates of net community production (NCP) in the oceanic mixed layer. The in situ O2/Ar&#8208;based method accounts for many physical factors that influence oxygen concentrations, permitting isolation of the biological oxygen signal produced by the balance of photosynthesis and respiration. However, this technique traditionally relies upon several assumptions when calculating the mixed&#8208;layer O2/Ar budget, most notably the absence of vertical fluxes of O2/Ar and the principle that the air&#8208;sea gas exchange of biological oxygen closely approximates net productivity rates. Employing a Lagrangian study design and leveraging data outputs from a regional physical oceanographic model, we conducted in situ measurements of O2/Ar in the California Current Ecosystem in spring 2016 and summer 2017 to evaluate these assumptions within a &#65533;worst&#8208;case&#65533; field environment. Quantifying vertical fluxes, incorporating nonsteady state changes in O2/Ar, and comparing NCP estimates evaluated over several day versus longer timescales, we find differences in NCP metrics calculated over different time intervals to be considerable, also observing significant potential effects from vertical fluxes, particularly advection. Additionally, we observe strong diel variability in O2/Ar and NCP rates at multiple stations. Our results reemphasize the importance of accounting for vertical fluxes when interpreting O2/Ar&#8208;derived NCP data and the potentially large effect of nonsteady state conditions on NCP evaluated over shorter timescales. In addition, diel cycles in surface O2/Ar can also bias interpretation of NCP data based on local productivity and the time of day when measurements were made.  
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  ISSN 2169-8953 ISBN Medium  
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  Call Number COAPS @ user @ Serial 1114  
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