JamBot Logo
1-59 of about 59 matches for site:pubs.giss.nasa.gov computed
https://pubs.giss.nasa.gov/abs/sm04100j.html
Pubs.GISS: Smith et al. 1989: Seasonal oceanic heat transports computed from an atmospheric model and ocean temperature... Go
https://pubs.giss.nasa.gov/abs/ji05300j.html
Pubs.GISS: Ji et al. 2023: Comparison between ozone column depths and methane lifetimes computed by one- and
https://pubs.giss.nasa.gov/abs/ro05010p.html
available potential energy (G z and G e ) as envisioned by Lorenz (1955) are computed on a global
https://pubs.giss.nasa.gov/abs/ca08400z.html
mixed layer (ML) and below it. Here R ρ and N are computed everywhere using the
https://pubs.giss.nasa.gov/abs/se03100m.html
SST of the tropical Pacific ocean. The upper ocean response is computed using a time
https://pubs.giss.nasa.gov/abs/sc00200p.html
4) on the basis of the qualitative differences between solar models computed using the compressible
https://pubs.giss.nasa.gov/abs/ba07400v.html
cloud properties are diagnosed using a MODIS simulator. Cloud droplet number concentrations (N) are computed identically from satellite-simulated
https://pubs.giss.nasa.gov/abs/li06210w.html
Quant. Spectrosc. Radiat. Transfer , 281 , 108080, doi:10.1016/j.jqsrt.2022.108080. Optical properties are computed for fractal
https://pubs.giss.nasa.gov/abs/mo01200v.html
The models provide consistent output, with errors (resulting from Monte Carlo statistical fluctuations) in computed irradiances that are seldom
https://pubs.giss.nasa.gov/abs/ma06400f.html
and the ensemble averages over the states become multidimensional integrations. These are computed using the Monte
https://pubs.giss.nasa.gov/abs/ca03620d.html
Program Hurricane Working Group. Diagnostics of standard measures of TC activity are computed from the recent
https://pubs.giss.nasa.gov/abs/dr03000u.html
equilibrium. July-September means of climate parameters relevant to TC genesis are computed from the simulations
https://pubs.giss.nasa.gov/abs/ri01010x.html
near-surface air temperature (GSAT) change. Efficacies are closest to one when ERF is computed using fixed sea surface
https://pubs.giss.nasa.gov/abs/ha02700w.html
on people and other parts of the biosphere, as shown by computed changes in the
https://pubs.giss.nasa.gov/abs/al09400v.html
the Mie theory. Fitting the observed rainbow with such a model (computed for a
https://pubs.giss.nasa.gov/abs/ko04500c.html
variability in Z α0-6 km , the mean extinction height diagnostic, as computed from the CALIOP
https://pubs.giss.nasa.gov/abs/bo06100c.html
and hence the electron density. Reasonable limits on the photoionization rate computed from recently proposed galactic
https://pubs.giss.nasa.gov/abs/al07000g.html
polynomials. As a practical example we compare extinction factors and asymmetry parameters computed for several
https://pubs.giss.nasa.gov/abs/ro00310j.html
available potential energy (G z and G e ) as formulated by Lorenz (1955) are computed on a global
https://pubs.giss.nasa.gov/abs/ca03200f.html
part of the nonlinear interactionsm, represented by a dynamical viscosity, is computed for a
https://pubs.giss.nasa.gov/abs/mi08500r.html
the appropriate river drainage basin on a 2°×2.5° resolution. The computed runoff depends on the
https://pubs.giss.nasa.gov/abs/vo03100n.html
comparison of measured bulk atmospheric and cloud properties to those computed in "trial
https://pubs.giss.nasa.gov/abs/wa01800d.html
ratio indices (MERIS chlorophyll a indices and the impurity index) were computed and compared
https://pubs.giss.nasa.gov/abs/ca04710r.html
the physical domain to the z where the fluxes are computed. In the
https://pubs.giss.nasa.gov/abs/cl02100m.html
occur during or shortly after core-contraction phases. Three simulations without an H-He interaction are computed to Fe
https://pubs.giss.nasa.gov/abs/ch01110q.html
reduce the computational burden. An atmospheric model containing aerosols and molecules is computed and added
https://pubs.giss.nasa.gov/abs/al08500g.html
into several modes and the respective effective radii and variances are computed. The methodology
https://pubs.giss.nasa.gov/abs/la04400t.html
within the Atmospheric Chemistry and Climate Model Intercomparison Project (ACCMIP). The computed deposition fluxes are compared
https://pubs.giss.nasa.gov/abs/ya02200w.html
is overestimated by a factor of 2 or more if advection is computed using the time
https://pubs.giss.nasa.gov/abs/po00100w.html
times the solar value. For Saturn two types of models were computed. One type of
https://pubs.giss.nasa.gov/abs/en08000i.html
introduced. A locally orthogonal polygonal grid, derived from the associated Voronoi diagram, is computed as the staggered
https://pubs.giss.nasa.gov/abs/ca05100g.html
of the two assumptions is required nor adjustable parameters are needed since ε ij is computed directly. The model
https://pubs.giss.nasa.gov/abs/mi07010j.html
size distribution. The agreement with observations is improved compared to previous distributions computed by either an older
https://pubs.giss.nasa.gov/abs/or04100o.html
ventilation of the stratosphere using one-way flux distributions. Robust transport diagnostics are computed using GEOSCCM subject to
https://pubs.giss.nasa.gov/abs/it01000b.html
matrix procedure. Using the corrected single-scattering parameters, reflectance (and emissivity) is computed via the invariant
https://pubs.giss.nasa.gov/abs/lu02000x.html
the Goddard Institute for Space Studies Atmosphere-Ocean Model (AOM). The computed trends of surface
https://pubs.giss.nasa.gov/abs/ch06210w.html
DISORT) at several wavenumbers. Radiances at other wavenumbers are interpolated based on the pre-computed total absorption and
https://pubs.giss.nasa.gov/abs/va06100c.html
is searched in a look-up table of simulated polarized reflectances computed for cloud
https://pubs.giss.nasa.gov/abs/or02100m.html
without being rendered ill defined by the short-τ eddy-diffusive singularity. Diagnostics are computed with an idealized circulation
https://pubs.giss.nasa.gov/abs/ma04110k.html
and precipitation at multiple timescales. We find that responses in models forced by pre-computed aerosol and ozone
https://pubs.giss.nasa.gov/abs/ma06100c.html
to obtain these distributions requires extensive computer CPU time, but only have to be computed once for a
https://pubs.giss.nasa.gov/abs/ma04010a.html
scattering and volume-absorption coefficients. Information content and microphysical parameter uncertainty is computed for full
https://pubs.giss.nasa.gov/abs/va05100g.html
closest fit in a look-up table of simulated polarized reflectances computed for cloud
https://pubs.giss.nasa.gov/abs/ca09200l.html
LES to the skewness of the velocity field which can be computed from the turbulence
https://pubs.giss.nasa.gov/abs/ch07500u.html
viscosity and the stochastic force of the improved subgrid model are computed from an analytical model
https://pubs.giss.nasa.gov/abs/ch03410n.html
the GCM. Instantaneous profiles of the lidar scattering ratio (SR) are first computed at the highest
https://pubs.giss.nasa.gov/abs/ma09110p.html
of Liquid Water Path (MAC-LWP) dataset (1988-2014) are compared to trends computed from the temporally
https://pubs.giss.nasa.gov/abs/en07000h.html
to address these issues. In each case, the horizontal acceleration is computed as an integration of
https://pubs.giss.nasa.gov/abs/ib02000c.html
c/a) in water, from which the scattering coefficient can be readily computed (b = c s - a
https://pubs.giss.nasa.gov/abs/in08000i.html
The gross moist stability (GMS), cloud-radiation feedback, and effective GMS were also computed for each
https://pubs.giss.nasa.gov/abs/ch09210z.html
6 for the other models. The degree of linear polarization computed by these RT codes
https://pubs.giss.nasa.gov/abs/ha01110v.html
the traditional instantaneous and adjusted forcings, Fi and Fa, with an easily computed alternative, Fs, yields a
https://pubs.giss.nasa.gov/year/1985.html
2. Russell, G.L. , J.R. Miller, and L.-C. Tsang, 1985: Seasonal oceanic heat transports computed from an atmospheric model
https://pubs.giss.nasa.gov/abs/ca01400w.html
and that entail a corresponding number of adjustable constants. These timescales are computed using renormalization group (RNG
https://pubs.giss.nasa.gov/year/1984.html
2. Siegel, P.H., and A.R. Kerr, 1984: The measured and computed performance of a
https://pubs.giss.nasa.gov/year/1983.html
2. Miller, J.R., G.L. Russell , and L.-C. Tsang, 1983: Annual oceanic heat transports computed from an atmospheric model
https://pubs.giss.nasa.gov/year/1989.html
CO;2. Smith, T.M., J.R. Miller, and G.L. Russell , 1989: Seasonal oceanic heat transports computed from an atmospheric model
https://pubs.giss.nasa.gov/authors/grussell.html
141-155. Smith, T.M., J.R. Miller, and G.L. Russell , 1989: Seasonal oceanic heat transports computed from an atmospheric model
https://pubs.giss.nasa.gov/year/2023.html
Marsh, and K. Tsigaridis , 2023: Comparison between ozone column depths and methane lifetimes computed by one- and