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3 edition of CTD measurements during 1997 and 1998 as part of the Global Ocean-Atmosphere-Land System (GOALS)/Pan American Climate Studies (PACS) found in the catalog.

CTD measurements during 1997 and 1998 as part of the Global Ocean-Atmosphere-Land System (GOALS)/Pan American Climate Studies (PACS)

CTD measurements during 1997 and 1998 as part of the Global Ocean-Atmosphere-Land System (GOALS)/Pan American Climate Studies (PACS)

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Published by U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Pacific Marine Environmental Laboratory, For sale by the National Technical Information Service in Seattle, Wash, Springfield, VA .
Written in English

    Subjects:
  • Ocean temperature -- Pacific Ocean -- Observations.,
  • Salinity -- Pacific Ocean -- Observations.,
  • Chemical oceanography -- Pacific Ocean -- Observations.,
  • Oceanography -- Pacific Ocean -- Observations.,
  • Hydrology -- Pacific Ocean -- Observations.,
  • Ocean-atmosphere interaction -- Pacific Ocean.

  • Edition Notes

    StatementK.E. McTaggart, G.C. Johnson.
    GenreObservations.
    SeriesNOAA data report ERL PMEL -- 66., Contribution no. 2050 from NOAA/Pacific Marine Environmental Laboratory, Contribution (Pacific Marine Environmental Laboratory (U.S.)) -- no. 2050.
    ContributionsJohnson, Gregory C., Pacific Marine Environmental Laboratory (U.S.), United States. National Oceanic and Atmospheric Administration.
    The Physical Object
    FormatMicroform
    Pagination2 v.
    ID Numbers
    Open LibraryOL17702092M

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    Relationships between El Nino-southern oscillation and the Arctic oscillation a climate-weather link. "Time series representing two of the climate systems' most leading variability in northern hemisphere, namely the El Nino-Southern Oscillation (ENSO) and the Arctic Oscillation (AO), together with 50 years of observed daily mean surface air temperature, precipitation over the . The International Comprehensive Ocean-Atmosphere Data Set (ICOADS) is a digital database of million weather observations made by ships, weather ships, and weather buoys spanning the years to The database was initially constructed in and continues to be expanded upon and updated on a regular basis. From the original data, gridded datasets were created.

      Abstract. In this paper, a study on phytoplankton dynamics and size in the tropical coastal waters of Singapore is presented. Chlorophyll-a levels in the Singapore Strait generally range from to 10 μg l –1, with an average value of μg l – general, higher chlorophyll concentrations are typically found off the east coast of Singapore, as well as in the shallower, Cited by: HP Series II computer allocates resources as warranted by the demands put on the system, small computer or the high-performance sector. 21 MX E-series computer. A and A, small desktop numeric data entry terminals. Components group: GaAs FETs (gallium arsenide field-effect transistors), the HFET


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CTD measurements during 1997 and 1998 as part of the Global Ocean-Atmosphere-Land System (GOALS)/Pan American Climate Studies (PACS) Download PDF EPUB FB2

CTD measurements during and as part of the Global Ocean-Atmosphere-Land System (GOALS)/Pan American Climate Studies (PACS) Author: K E McTaggart ; Gregory C Johnson ; Pacific Marine Environmental Laboratory (U.S.).

CTD measurements during and as part of the Global Ocean-Atmosphere-Land System (GOALS)/Pan American Climate Studies (PACS) Published Date: CTD measurements during and as part of the Global Ocean -Atmosphere-Land System (GOALS)/Pan American Climate Studies (PACS).

NOAA Data Report ERL PMEL, pp. Merle, J., Rotschi, H., & Voituriez, B. Zonal circulation in the tropical western South Pacific at °E. CTD measurements during and as part of the Global Ocean-Atmosphere-Land System (GOALS)/Pan American Climate Studies (PACS).

NOAA Data Report ERL PMEL, pp. + McTaggart, K. Johnson, C. Fleurant, and M. Baringer. CTD measurements during and as part of the Global Ocean–Atmosphere–Land System (GOALS)/Pan American Climate Studies (PACS).

NOAA Data Report ERL PMEL, pp. NOAA Data Report ERL PMEL, by: Get this from a library. CTD measurements during and as part of the Global Ocean-Atmosphere-Land System (GOALS) Pan American Climate Studies (PACS). [K E McTaggart; Pacific Marine Environmental Laboratory (U.S.);]. Ctd Measurements During And As Part Of The Global Ocean-Atmosphere-Land System (goals)/pan American Climate Studies (pacs) Article (PDF Available) January with 63 Reads How we.

K. McTaggart and G. Johnson, CTD Measurements During and as Part of the Global Ocean-Atmosphere-Land System (GOALS)/PAN American Climate Studies (PACS) (NOAA Data Report ERL, PMELB, Seattle, Washington, ), Vol.

Author: V. Sosnin. The Flexible Global Ocean-Atmosphere-Land System model, Spectral Version 2 (FGOALS-s2) was used to simulate realistic climates and to study anthropogenic influences on climate change.

Specifically, the FGOALS-s2 was integrated with Coupled Model Intercomparison Project Phase 5 (CMIP5) to conduct coordinated experiments that will provide valuable Cited by: [1] A global simulation of the ocean response to atmospheric wind and pressure forcing has been run during the Topex/Poseidon (T/P) period (–), using a new hydrodynamic finite element (FE) model, MOG2D‐G.

Model outputs are compared to in situ observations with tide gauge data (TG) and bottom pressure gauge data (BPR), and also with T/P altimetric cross Cited by: Interspersed within the main observing system data are high‐quality bottle and CTD temperature measurements from projects such as WOCE (–).

Historic studies of ocean heat content and other related variables need to take into consideration the changes in the observing system and the limitations of the system during each time period Cited by:   4. Lamborg, C. H., Fitzgerald, W. F., O'Donnell, J.

& Torgersen, T. A non-steady-state compartmental model of global-scale mercury biogeochemistry with. Coupled ocean-atmosphere dynamics in the Indian Ocean during Webster PJ(1), Moore AM, Loschnigg JP, Leben RR.

Author information: (1)Program in Atmospheric and Oceanic Sciences, Campus BoxUniversity of Colorado, Boulder, ColoradoUSA. [email protected] Comment in Nature. Sep 23;()Cited by: forcing (i.e., the change in the global mean net radiative flux at the tropopause holding all other inputs to the radiative transfer fixed) under this scenario is W m 2 [IPCC Third Assessment Report (Ramaswamy et al.

) Tables and ). The uncertainty in forc-ings is estimated to be 10% for the period – often used in global warming studies in which the ocean acts only as a heat capacitor--and has no active dynamics--is not discussed.

For climate time scales, a division of the coupled system at the ocean-atmosphere interface is not easy to defend. Incoming solar (shortwave).

McTaggart, K.E. and G.C. Johnson, CTD measurements during and as part of the Global Ocean-Atmosphere-Land System (GOALS)/ Pan American Climate Studies (PACS).

NOAA Data Report ERL PMEL (2 vols.), Seattle, Washington, pp. The coupled ocean-atmosphere general circulation model (CGCM) used in this study is the primary version of a Flexible General Circulation Model for climate system (referred to as FGCM-0). The FGCM-0 is formulated based on the NCAR CSM-1 (Boville and Gent, ) by replacing the CSM-1's ocean component, NCOM (the NCAR CSM Ocean Model), with the.

Introduction. This paper describes the design and performance of the ZEUS Second-Level Trigger for the Central Tracking Detector (CTD-SLT). ZEUS is a multipurpose detector, designed to record the final state particles of collisions between GeV protons and 30 GeV electrons 5 at the `Hadron Elektron Ring Anlage’ (HERA) at DESY.

Its main elements are an inner tracking system Cited by: 3. Low degree gravitational changes from earth rotation and geophysical models. parently associated with the / El Nin (EOP C04), Flexible Global Ocean-Atmosphere-Land System Model. CTD measurements during and as part of the Equatorial Pacific Ocean Climate Studies (EPOCS) Published Date: Series: NOAA.

The CTD acts as a platform for assembly of factors that regulate transcription initiation, elongation, termination, and mRNA processing.

Pol II with a hypophosphorylated CTD is initially recruited to promoters during PIC formation and is phosphorylated at Ser5 during Cited by: GOALS (Global Ocean-Atmosphere-Land System) for Predicting Seasonal-to-Interannual Climate: A Program of Observation, Modeling, and Analysis. Washington, DC: The National Academies Press.

doi: / ×.The wintertime Arctic temperature (T, surface hPa) decreased from and increased rapidly fromin contrast to the global mean surface air temperature. Here we examine aspects of circulation variability that are associated with these temperature changes using the NCEP/NCAR and ERA-Interim reanalysis products.