Sentences with phrase «ocean model naosim»

To roughly solve the problem you use a moist air and ocean model applying basic thermodynamics and compare that to a radiant model since the surface is the issue.

To force an ensemble of ocean model experiments I would like to use (near) surface data from individual members of the 20CR.

Ocean Model., 113, 131 - 144.

Sun, S., and R. Bleck, 2001: Atlantic thermohaline circulation and its response to increasing CO2 in a coupled atmosphere - ocean model.

P.S. conducted and analysed the ocean model experiments, S.M. analysed the observational data.

Even a simple ocean model usually has a number of slightly different equilibria actually, due to shifts in the location of convective activity (by a few grid boxes - I'm not talking here about a big reorganisation of the circulation).

However from the paper quoted, «Cool - skin simulation by a one - column ocean model — Chia - Ying Tu and Ben - Jei Tsuang», diffusion is stated as being the «only» mechanism.

This was the point of Part Three in the series and is also noted under Ocean Model point 5 in this article.

«(3) ocean model simulations (e.g., Le Quéré et al., 2003; McKinley et al., 2004a) and (4) terrestrial carbon cycle and coupled model simulations (e.g., C. Jones et al., 2001; McGuire et al., 2001; Peylin et al., 2005; Zeng et al., 2005).»

Here's a 2005 paper which is freely available — Cool - skin simulation by a one - column ocean model, by Chia - Ying Tu and Ben - Jei Tsuang.

(S7) using a coupled atmosphere - ocean model.

Rind, D., G.L. Russell, G.A. Schmidt, S. Sheth, D. Collins, P. Demenocal, and J. Teller, 2001: Effects of glacial meltwater in the GISS Coupled Atmosphere - Ocean Model: Part II: A bi-polar seesaw in Atlantic Deep Water production.

Lucarini, V., and G.L. Russell, 2002: Comparison of mean climate trends in the Northern Hemisphere between National Centers for Environmental Prediction and two atmosphere - ocean model forced runs.

We use the simplified atmosphere — ocean model of Russell et al. [108], which solves the same fundamental equations (conservation of energy, momentum, mass and water substance, and the ideal gas law) as in more elaborate global models.

Sun, S., and R. Bleck, 2001: Thermohaline circulation studies with an isopycnic coordinate ocean model.

Results with a large - scale coupled ice - ocean model [Zhang and Steele, 2007] suggest the appropriate model background mixing for the Arctic Ocean is an order of magnitude lower than for ice - free oceans.

Cox (1975)(«the most ambitious ocean simulation so far,» according to W.L. Gates, p. 116); published at the same time was a somewhat cruder whole - ocean model, aimed at integration with the Mintz - Arakawa model, Takano (1975); Manabe et al. (1975), quote p. 3; together with Bryan et al. (1975); further landmarks included Manabe et al. (1979); Washington et al. (1980).

The 60 level ocean model is coupled with the sea - ice component and uses a horizontal resolution of approximately 3 ° with a displaced North Pole.

A standard approach is to emulate with an upwelling diffusive ocean model.

Kauker et al., (AWI / OASys); 3.72 (3.30 - 4.14), Modeling Estimated from ensemble coupled sea ice - ocean model runs based on atmospheric reanalyses fields from 1994 - 2013.

She and colleagues at the Massachusetts Institute of Technology in Cambridge, Massachusetts used the NASA GISS ocean model and the MIT General Circulation Model to simulate one of the Atlantic's major current systems that delivers absorbed heat and gases to the depths.

Jin (IARC), 4.62, Modeling (ice - ocean)(Same as June) A coupled ice - ocean model (POP - CICE) forecast of the September sea ice extent minimum.

To get all the good out of the proxies you would either need extremely long averaging or one kick butt ocean model.

Our atmosphere - ocean model shows that the freshwater spurs amplifying feedbacks that would accelerate ice shelf and ice sheet mass loss, thus providing support for our assumption of a nonlinear ice sheet response.

Well he developed a 3D ocean model and built the computer to run the model, so I daresay he knows more about ocean dynamics than the one who keeps misrepresenting the work of Tsonis et al..

An ocean model?

Time series of AMOC anomaly at 1000 m depth at 45 ° N (top panels) and 26.5 ° N (bottom panels) for the set of ocean reanalysis products (left panels) and the set of No Assimilation forced ocean model simulations (right panels).

Each atmospheric version is coupled to two different ocean general circulation models: the Russell ocean model (GISS - E2 - R) and HYCOM (GISS - E2 - H).

This version, released in December 1990, became known as Modular Ocean Model v1.0 (MOM1).

Our research centers around the ocean model HYCOM with ecosystem applications (HYCOM - NORWECOM and HYCOM - ECOSMO).

The Modular Ocean Model (MOM) is a three - dimensional ocean circulation model designed primarily for studying the ocean climate system.

The figure at the top from Golaz et al, 2013 shows simulations from three versions of the CM3 coupled atmosphere - ocean model developed at GFDL (Donner, et al 2011).

In particular, initial stages of atmospheric model development often take place without coupling to an ocean model, running instead over observed sea surface temperatures (SSTs) and sea ice extent.

The biggest point it should make is that attempting to estimate sensitivity to CO2 with paleo is a waste of time without one kick butt ocean model.

In an earlier study (Labe et al., 2018a), we show that the CESM - LENS sea ice thickness compares well with satellite observations and output from an ice - ocean model.

Our method uses estimates of ice thickness from a coupled ice - ocean model as predictors for a statistical forecast of the minimum ice extent in September.

The method is a sea ice - ocean model ensemble run (without and with assimilation of sea - ice / ocean observations); the coupled ice - ocean model NAOSIM has been forced with atmospheric surface data from January 1948 to 7 July 2015.

Ice - ocean model simulations, on the other hand, have requirements with respect to data density and quality, e.g., for observed ice thickness fields used in initialization of model runs, that are currently not being met by existing data sources (with the exception of, e.g., satellite - observed ice concentration fields).

The prediction is made from an ice / ocean model estimate of the state of the system at the end of April 2008.

The close relationship that exists between the dynamic height and the mass field of the ocean allows these two parameters to be used within a two - layer reduced gravity ocean model to monitor the upper layer thickness (Goni et al., 1996), which is defined in this study to go from the sea surface to the depth of the 20 °C isotherm.

Kauker et al, 4.5, + / - 0.4, Model Sea ice - ocean model ensemble run - For a more detailed description we refer to our July report.

I'm assuming that there is a coupled ocean model.

All runs are conducted using preindustrial (1850) land use conditions in order to conform with our best - available slab ocean model data; however the orbital conditions are set for the year 2000.

The slab ocean model is a computationally efficient scheme that allows sea surface temperatures to interact with the atmosphere; and is necessary for propagating energy imbalances due to land cover change that lead to shifts in precipitation.

The ocean model offers a spatial resolution of 1.5 ˚ × 3.5 ˚ and is vertically divided into 40 unevenly spaced layers, with model poles placed over Greenland and Antarctica.

Sea ice formation and dynamics are simulated in the ocean model.

The ocean model is in a sense a module parallel to that of the atmosphere in treating the transports of heat, salinity, and water / ice.

Then the authors use the observed, or more accurately described «reconstructed,» flux anomalies over the Arctic for the past three decades to force a forward ocean model.

The task team will also coordinate with the U.S. CLIVAR Decadal Predictability Working Group as well as the CLIVAR Working Group on Ocean Model Development and CLIVAR Global Synthesis and Observational Panel.

It is not clear whether the bias is caused by an imperfect sea ice - ocean model or by imperfect initial or boundary conditions.