Institution
Geophysical Fluid Dynamics Laboratory
Facility•Princeton, New Jersey, United States•
About: Geophysical Fluid Dynamics Laboratory is a facility organization based out in Princeton, New Jersey, United States. It is known for research contribution in the topics: Climate model & Climate change. The organization has 525 authors who have published 2432 publications receiving 264545 citations. The organization is also known as: GFDL.
Topics: Climate model, Climate change, Sea surface temperature, Tropical cyclone, Thermohaline circulation
Papers published on a yearly basis
Papers
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TL;DR: In this article, an empirical relation is developed to express the total ozone mapping spectrometer (TOMS) aerosol index (AI) for the case of dust plumes, as an explicit function of four physical quantities: the single scattering albedo, optical thickness, altitude of the plume and surface pressure.
Abstract: [1] An empirical relation is developed to express the Total Ozone Mapping Spectrometer (TOMS) aerosol index (AI) for the case of dust plumes, as an explicit function of four physical quantities: the single scattering albedo, optical thickness, altitude of the plume and surface pressure. This relation allows sensitivity analysis of the TOMS AI with physical properties, quantitative comparison with dust model results and physical analysis of dust sources, without the necessity of cumbersome radiative calculation. Two applications are presented: (1) the case study of a dust storm over the North Atlantic in March 1988, and (2) the characterization of 13 major dust sources. The first application shows that simulated dust distribution can be quantitatively compared to TOMS AI on a daily basis and over regions where dust is the dominant aerosol. The second application necessitates to further parameterize the relation by replacing the optical thickness and the altitude of the plume by meteorological variables. The advantage is that surface meteorological fields are easily available globally and for decades but the formulation only applies to dust sources. The daily, seasonal and interannual variability of the parameterized index over major dust sources reproduces correctly the variability of the observed TOMS AI. The correlation between these two indices is used to determine the surface characteristics and physical properties of dust aerosol over the sources.
74 citations
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TL;DR: In this article, the authors generalized space-time spectral formulas to partition the time power spectrum of transient disturbances consisting of multiple wavenumbers into standing and traveling parts by assuming that these parts are incoherent with each other.
Abstract: Space-time spectral formulas are generalized to partition the time power spectrum of transient disturbances consisting of multiple wavenumbers into standing and traveling parts by assuming that these parts are incoherent with each other. This technique is useful in interpreting the spatial variation of wave amplitude in terms of standing and traveling waves. An example of its application to the analysis of transient planetary waves is given.
74 citations
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TL;DR: In this article, the rotation rate, obliquity and diurnal period of an Earth-like model atmosphere produces a wide range of circulation forms, some of which resemble those observed on Venus, Mars, Jupiter, Saturn and (perhaps) on Uranus and Neptune.
Abstract: Altering the rotation rate, obliquity and diurnal period of an Earth-like model atmosphere produces a wide range of circulation forms, some of which resemble those observed on Venus, Mars, Jupiter, Saturn and (perhaps) on Uranus and Neptune. These unified solutions suggest: that Jupiter and Saturn resemble a larger, faster-spinning Earth and possess a stress-bearing or momentum-exchanging sublayer-, that easterly winds prevail in Uranus' summer hemisphere; and that Venus resembles a slowly rotating Earth if diurnal heating variations are included.
74 citations
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TL;DR: In this article, the authors investigated the time lags between changes in radiative forcing and the resulting simulated climate responses in a set of transient climate change experiments and concluded that much of the warming due to current greenhouse gas levels is yet to be realized.
Abstract: Time lags between changes in radiative forcing and the resulting simulated climate responses are investigated in a set of transient climate change experiments. Both surface air temperature (SAT) and soil moisture responses are examined. Results suggest that if the radiative forcing is held fixed at today's levels, the global mean SAT will rise an additional 1.0K before equilibrating. This unrealized warming commitment is larger than the 0.6K warming observed since 1900. The coupled atmosphere-ocean GCM's transient SAT response for the year 2000 is estimated to be similar to its equilibration response to 1980 radiative forcings—a lag of ∼20 years. Both the time lag and the warming commitment are projected to increase in the future, and depend on the model‧s climate sensitivity, oceanic heat uptake, and the forcing scenario. These results imply that much of the warming due to current greenhouse gas levels is yet to be realized.
74 citations
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TL;DR: In this article, the authors studied the relationship between the dominant patterns of sea surface temperature variability in the North Pacific and the North Atlantic and found that the correlations are significant when the Pacific Decadal Oscillation (PDO) leads the AMO by 1 year.
Abstract: We studied the relationship between the dominant patterns of sea surface temperature (SST) variability in the North Pacific and the North Atlantic. The patterns are known as the Pacific Decadal Oscillation (PDO) and the Atlantic Multi-decadal Oscillation (AMO). In the analysis we used two different observational data sets for SST. Due to the high degree of serial correlation in the PDO and AMO time series, various tests were carried out to assess the significance of the correlations. The results demonstrated that the correlations are significant when the PDO leads the AMO by 1 year and when the AMO leads the PDO by 11–12 years. The possible physical processes involved are discussed, along with their potential implication for decadal prediction.
74 citations
Authors
Showing all 546 results
Name | H-index | Papers | Citations |
---|---|---|---|
Alan Robock | 90 | 346 | 27022 |
Isaac M. Held | 88 | 215 | 37064 |
Larry W. Horowitz | 85 | 253 | 28706 |
Gabriel A. Vecchi | 84 | 282 | 31597 |
Toshio Yamagata | 83 | 294 | 27890 |
Li Zhang | 81 | 727 | 26684 |
Ronald J. Stouffer | 80 | 153 | 56412 |
David Crisp | 79 | 328 | 18440 |
Thomas L. Delworth | 76 | 178 | 26109 |
Syukuro Manabe | 76 | 129 | 25366 |
Stephen M. Griffies | 68 | 202 | 18065 |
John Wilson | 66 | 487 | 22041 |
Arlene M. Fiore | 65 | 168 | 17368 |
John P. Dunne | 64 | 189 | 17987 |
Raymond T. Pierrehumbert | 62 | 192 | 14685 |