1-100 of about 136 matches for site:www.giss.nasa.gov site:www.giss.nasa.gov site:www.giss.nasa.gov determine
Pubs.GISS: Marchand et al. 2016: Reserves and trade jointly determine exposure to food supply shocks
https://www.giss.nasa.gov/pubs/abs/ma02210s.html
Pubs.GISS: Marchand et al. 2016: Reserves and trade jointly determine exposure to food supply shocks Go
Pubs.GISS: Lacis and Matsushima 1966: Method of correction for instrumental astigmatism to determine
https://www.giss.nasa.gov/pubs/abs/la07200r.html
and Matsushima 1966: Method of correction for instrumental astigmatism to determine the center
Pubs.GISS: Hickman et al. 2023: Emissions background, climate, and season determine the impacts of p
https://www.giss.nasa.gov/pubs/abs/hi04300i.html
Pubs.GISS: Hickman et al. 2023: Emissions background, climate, and season determine the impacts of past
https://www.giss.nasa.gov/pubs/abs/kn08100v.html
properties using polarimetric, multiple view angle, and multi spectral observations, and therefore determine DCF from aerosols above
https://www.giss.nasa.gov/pubs/abs/co05010b.html
of wavelength and phase angle. Such measurements can be used to determine whether aerosols are spherical
Pubs.GISS: Collins 1978: Analysis of airborne spectroradiometric data and the use of Landsat data fo
https://www.giss.nasa.gov/pubs/abs/co03400p.html
generated by the airborne system are used, in particular, to determine the spectral
Pubs.GISS: Knobelspiesse et al. 2015: Cloud thermodynamic phase detection with polarimetrically sens
https://www.giss.nasa.gov/pubs/abs/kn04200y.html
if ground-based visible and near-infrared passive radiometers that have polarization sensitivity can determine the thermodynamic
https://www.giss.nasa.gov/pubs/abs/ru07000g.html
sunlight in ten spectral channels between 410 and 945 nm to determine the physical
Pubs.GISS: LeGrande 2006: The Climate Imprint on the Oxygen Isotopic Composition of Water: Observati
https://www.giss.nasa.gov/pubs/abs/le01200l.html
precip . Temperature and δ 18 O seawater (regionally linearly related to salinity) determine δ 18 O calcite
https://www.giss.nasa.gov/pubs/abs/mi06810d.html
operated scientific laboratories at the NASA Goddard Space Flight Center (GSFC) and determine the effects
Pubs.GISS: Geogdzhayev et al. 2021: Calibration of the DSCOVR EPIC visible and NIR channels using mu
https://www.giss.nasa.gov/pubs/abs/ge09200d.html
temporarily and spatially collocated with EPIC observations. These scenes are used to determine reflectance to count
Pubs.GISS: Mishchenko and Travis 1997: Satellite retrieval of aerosol properties over the ocean usin
https://www.giss.nasa.gov/pubs/abs/mi08000d.html
sensing of tropospheric aerosols relies upon radiance measurements that are interpreted using algorithms that determine best fits to
https://www.giss.nasa.gov/pubs/abs/li05100g.html
to separate clear/cloudy skies and warm/cold clouds and to determine cloud optical thickness, cloud
https://www.giss.nasa.gov/pubs/abs/ca05810h.html
potentials are almost identical to the nucleon-nucleon case. Computations to determine whether neutrons can solidify
Pubs.GISS: Knobelspiesse 2010: Atmospheric Aerosol Optical Property Retrieval with Scanning Polarime
https://www.giss.nasa.gov/pubs/abs/kn07100z.html
success. The software is very flexible, and was also used to determine the sensitivity
Pubs.GISS: Green 1974: Sources of error and expected accuracy in ab initio one-electron operator pro
https://www.giss.nasa.gov/pubs/abs/gr04010a.html
such as the molecular quadrupole moment which is not so easy to determine experimentally, can then be
https://www.giss.nasa.gov/pubs/abs/ba01400g.html
in order to study their stability against pulsation; that is, to determine whether a small
https://www.giss.nasa.gov/pubs/abs/ro06400f.html
delimit the geographical extent of the crop and they determine in large
Pubs.GISS: Le Marshall et al. 1999: Satellite calibration using a collocated nadir observation techn
https://www.giss.nasa.gov/pubs/abs/ma02410m.html
problems inherent in the absolute calibration of satellite instruments. Orbital calculations determine where and when
Pubs.GISS: Austin et al. 2003: Uncertainties and assessments of chemistry-climate models of the stra
https://www.giss.nasa.gov/pubs/abs/au01000b.html
values in the models. The results are also compared to determine the possible
https://www.giss.nasa.gov/pubs/abs/la05300q.html
atom in a simple cubic structure, using one-particle Green's functions. We determine the accuracy
https://www.giss.nasa.gov/pubs/abs/ri09400v.html
of the GISS 9 level climate model. Additional experiments are run to determine how the middle
https://www.giss.nasa.gov/pubs/abs/do08300m.html
solar-flare model. The object of this paper is to determine what new information about
https://www.giss.nasa.gov/pubs/abs/pe03500c.html
through the provision of new data and tools that better determine risk factors. In
Pubs.GISS: Zhou et al. 2018: Simulation of mesoscale cellular convection in marine stratocumulus. Pa
https://www.giss.nasa.gov/pubs/abs/zh06200a.html
sub-cloud moist cold pools surprisingly tends to respond to, rather than determine, the mesoscale
Pubs.GISS: Adames et al. 2017: Characterization of moist processes associated with changes in the pr
https://www.giss.nasa.gov/pubs/abs/ad01100l.html
an increase in the mean horizontal moisture gradients. The terms that determine the strength
https://www.giss.nasa.gov/pubs/abs/ro08300g.html
a bispectral threshold is then used as the last step to determine the cloud
https://www.giss.nasa.gov/pubs/abs/hu02200w.html
tool in water isotope systematics, and it is thus important to determine to what
https://www.giss.nasa.gov/pubs/abs/ac07000g.html
2 , but it is difficult to estimate because the physical processes that determine global aerosol and
Pubs.GISS: Pang et al. 1979: Voyager 1 photopolarimeter experiment and the phase curve and surface m
https://www.giss.nasa.gov/pubs/abs/pa01300e.html
Ganymede. Nature , 280 , 804-806, doi:10.1038/280804a0. Optical wavelength photometry used to determine the surface
Pubs.GISS: Tsigaridis and Kanakidou 2003: Global modelling of secondary organic aerosol in the tropo
https://www.giss.nasa.gov/pubs/abs/ts00200p.html
formation. A number of global simulations have been performed to determine a possible
https://www.giss.nasa.gov/pubs/abs/la01400w.html
use the isotropic part of the atom-atom potential to determine the trajectories
https://www.giss.nasa.gov/pubs/abs/wi01300e.html
in the brightness and the radial velocity are analyzed to determine the characteristics
https://www.giss.nasa.gov/pubs/abs/de00900m.html
direct capture, and background levels. Additional experimental measurements are therefore needed to determine if 19 F(p
Pubs.GISS: Behrenfeld et al. 2019: The North Atlantic Aerosol and Marine Ecosystem Study (NAAMES): S
https://www.giss.nasa.gov/pubs/abs/be06200a.html
phases of the annual cycle and their dependence on environmental forcings, (2) determine how these phases interact
Pubs.GISS: Tselioudis and Rossow 2006: Climate feedback implied by observed radiation and precipitat
https://www.giss.nasa.gov/pubs/abs/ts01100t.html
changes with climate-warming predicted by a climate model are used to determine the radiation
https://www.giss.nasa.gov/pubs/abs/ca07620h.html
exoplanetary system properties, including "external" exoplanet parameters (e.g., mass and radius), to determine an exoplanet's suitability
https://www.giss.nasa.gov/pubs/abs/da09000a.html
Columbia CO survey of the first Galactic quadrant was used to determine the locations
Pubs.GISS: Cook et al. 2011: Forced and unforced variability of twentieth century North American dro
https://www.giss.nasa.gov/pubs/abs/co01500p.html
to SST forcing. We use a large ensemble statistical modeling approach to determine how successfully we can
https://www.giss.nasa.gov/pubs/abs/gr09900h.html
clouds found in the first and second quadrants to determine how the Carina
https://www.giss.nasa.gov/pubs/abs/sh04800g.html
of aerosols in India's monsoon precipitation and (2) to determine the roles
https://www.giss.nasa.gov/pubs/abs/ca01920f.html
Rackham to observe the Moon in order to determine whether a similar
Pubs.GISS: Durham et al. 1989: Comparative analysis of the atmospheres of early Earth and early Mars
https://www.giss.nasa.gov/pubs/abs/du00100w.html
masses. We then use a one-dimensional radiative-convective atmospheric model to determine if a 1
https://www.giss.nasa.gov/pubs/abs/gr08500r.html
model ECHAM4.L39(DLR)/CHEM two specific chemistry-transport interactions are investigated aiming to determine their importance for
https://www.giss.nasa.gov/pubs/abs/ca00310j.html
parameter as we did in the case of elliptical galaxies, we determine it by requiring that
https://www.giss.nasa.gov/pubs/abs/st03900e.html
approach is used to study the time-dependent problem and determine how long it would
https://www.giss.nasa.gov/pubs/abs/ma07310h.html
To accurately predict how much warmer climate change will make the earth, scientists must determine the infl
https://www.giss.nasa.gov/pubs/abs/gr02800o.html
10.1016/0022-2852(77)90261-2. Ab initio calculations are carried out to determine γΠ (true), the
https://www.giss.nasa.gov/pubs/abs/li07100z.html
181, doi:10.1007/BF00200849. The Voyager Photopolarimeter Experiment is designed to determine the physical
Pubs.GISS: Dymond et al. 2005: Using satellite fire detection to calibrate components of the Fire We
https://www.giss.nasa.gov/pubs/abs/dy06000k.html
In response, fire management systems are being developed. This study set out to determine the relationships
Pubs.GISS: Thompson et al. 2020: Quantifying uncertainty for remote spectroscopy of surface composit
https://www.giss.nasa.gov/pubs/abs/th03200x.html
to absolute units, invert physical models to estimate atmospheric effects, and then determine surface properties from the
Pubs.GISS: Dame and Thaddeus 1985: A wide-latitude CO survey of molecular clouds in the northern Mil
https://www.giss.nasa.gov/pubs/abs/da04000r.html
of these with optical objects (dark nebulae, OB associations, etc.), and to determine distances and masses
Pubs.GISS: Kassamba-Diaby et al. 2023: The chemical characteristics of rainwater and wet atmospheric
https://www.giss.nasa.gov/pubs/abs/ka06400u.html
and global impacts on ecosystems, it is of crucial importance to determine rain chemical composition and
https://www.giss.nasa.gov/pubs/abs/ar07100r.html
equilibrium temperature profile in planetary atmospheres. In order to accurately determine these effects, a
Pubs.GISS: Leboissetier et al. 2005: Consistent large-eddy simulation of a temporal mixing layer lad
https://www.giss.nasa.gov/pubs/abs/le06100c.html
model coefficient. The ability of the dynamic models to determine the model
Pubs.GISS: Cook and Buckley 2009: Objective determination of monsoon season onset, withdrawal, and l
https://www.giss.nasa.gov/pubs/abs/co05400j.html
mainland Thailand, we apply a two-phase linear regression model to objectively determine the onset
Pubs.GISS: Schmidt and Mysak 1996: The stability of a zonally averaged thermohaline circulation mode
https://www.giss.nasa.gov/pubs/abs/sc04000r.html
combination of analytical and numerical techniques are used to efficiently determine the qualitative
https://www.giss.nasa.gov/pubs/abs/st04120g.html
P (overshoot distance divided by local pressure scale height) in order to determine in more
Pubs.GISS: Shindell et al. 2024: Premature deaths due to heat exposure: The potential effects of nei
https://www.giss.nasa.gov/pubs/abs/sh03900p.html
scale of acclimatization, more neighborhood-level epidemiological data are urgently needed to determine the health
https://www.giss.nasa.gov/pubs/abs/gr01010m.html
focus on the feasibility of the MODIS sensor to determine aerosol optical depth. In
Pubs.GISS: Janssen et al. 2005: Microwave remote sensing of Jupiter's atmosphere from an orbiting sp
https://www.giss.nasa.gov/pubs/abs/ja06000k.html
off-nadir emission angles, combined with absolute brightness temperature measurements, can allow us to determine the global
https://www.giss.nasa.gov/pubs/abs/fe07000g.html
A 40 × scale model of the mixer block was used to determine the experimental
Pubs.GISS: Črnivec et al. 2023: Evaluating the representation of tropical stratocumulus and s
https://www.giss.nasa.gov/pubs/abs/cr02100m.html
represents the basis for improving parameterizations of physical processes that determine the cloud
https://www.giss.nasa.gov/pubs/abs/ca08510t.html
times smaller than its value at low energies. From this we are able to determine the scale
https://www.giss.nasa.gov/pubs/abs/de08200o.html
general circulation. The local balance between precipitation and evaporation over ocean helps determine the thermohaline
Pubs.GISS: Ballard et al. 2014: Hydroclimate variability and change in the Prairie Pothole Region, t
https://www.giss.nasa.gov/pubs/abs/ba06400u.html
phase 5 of the Coupled Model Intercomparison Project are used to determine whether a recent
https://www.giss.nasa.gov/pubs/abs/ca08610m.html
abundance of boron is of considerable interest, but is difficult to determine. Boron undergoes thermonuclear destruction
Pubs.GISS: Park et al. 2023: Herbarium records provide reliable phenology estimates in the understud
https://www.giss.nasa.gov/pubs/abs/pa04700w.html
surveys) and herbarium specimens at various spatial and taxonomic scales to determine whether specimens can provide
https://www.giss.nasa.gov/pubs/abs/mi05910b.html
appearence of the spiral patterns. Several experiments were carried out to determine the roles
Pubs.GISS: Camargo et al. 2020: Characteristics of model tropical cyclone climatology and the large-
https://www.giss.nasa.gov/pubs/abs/ca02720m.html
Therefore, other processes associated with the model physics, dynamical core, and resolution determine the climatological
Pubs.GISS: Gao et al. 2018: Sedimentation efficiency of condensation clouds in substellar atmosphere
https://www.giss.nasa.gov/pubs/abs/ga05200z.html
Marley (2001) that relies on a sedimentation efficiency parameter, f sed , to determine the vertical
Pubs.GISS: Holzer 2009: The path density of interhemispheric surface-to-surface transport. Part I: D
https://www.giss.nasa.gov/pubs/abs/ho03400p.html
be computed. A simple algorithm for using passive tracers to determine η is developed. A
https://www.giss.nasa.gov/pubs/abs/go01000b.html
sea-level rise), rather than a single global mean sea-level trend, that will determine each locality's vulnerability
Pubs.GISS: Gao et al. 2018: Retrieval of aerosol properties and water-leaving reflectance from multi
https://www.giss.nasa.gov/pubs/abs/ga06200a.html
dissolved organic matter (CDOM) and non-algal particles (NAP). Our retrieval algorithm can accurately determine the water
https://www.giss.nasa.gov/pubs/abs/ri07700f.html
system. Three different configurations of sea surface temperatures are used to help determine whether the tropospheric
https://www.giss.nasa.gov/pubs/abs/me08000d.html
367-396, doi:10.1023/A:1005358130291. Our central goal is to determine the importance
Pubs.GISS: Harries and Futyan 2006: On the stability of the Earth's radiative energy balance: Respon
https://www.giss.nasa.gov/pubs/abs/ha08110y.html
radiative fields to the eruption of Mt Pinatubo to determine time constants for
Pubs.GISS: Field et al. 2010: Effects of post-condensation exchange on the isotopic composition of w
https://www.giss.nasa.gov/pubs/abs/fi06100c.html
doi:10.1029/2010JD014334. We conducted experiments with an atmospheric general circulation model to determine the effects
Pubs.GISS: Menzel et al. 2024: Replicating the Hadley Cell and subtropical jet disconnect in idealiz
https://www.giss.nasa.gov/pubs/abs/me04300i.html
use meteorological reanalysis, comprehensive climate models, and an idealized atmospheric model to determine the necessary
https://www.giss.nasa.gov/pubs/abs/to03200x.html
CO 2 ) concentrations, together with projected variations in temperature and precipitation will determine future agricultural production. Estimates
Pubs.GISS: Poore et al. 1995: Cloud layer thicknesses from a combination of surface and upper-air ob
https://www.giss.nasa.gov/pubs/abs/po07000g.html
63 sites in the Northern Hemisphere. Rawinsonde observations are employed to determine the locations
https://www.giss.nasa.gov/pubs/abs/ga05100g.html
The initial composition of dust and its chemical transformations during transport determine the way
https://www.giss.nasa.gov/pubs/abs/mc01000b.html
647-656, doi:10.1086/160200. Accurate theoretical collisional excitation rates are used to determine the emissivities
https://www.giss.nasa.gov/pubs/abs/mi09300d.html
The computations are carried out by using the atmospheric model to determine the net
https://www.giss.nasa.gov/pubs/abs/ri04600x.html
are needed, especially in the vicinity of forests, to determine appropriate parameterizations. Go to
Pubs.GISS: Guarin et al. 2019: Impacts of tropospheric ozone and climate change on Mexico wheat prod
https://www.giss.nasa.gov/pubs/abs/gu05100p.html
future O 3 concentrations on wheat production in Mexico are unknown. To determine these impacts, the
Pubs.GISS: Stone et al. 2013: Evaluation of ISCCP multisatellite radiance calibration for geostation
https://www.giss.nasa.gov/pubs/abs/st09020f.html
range, the results suggest that the ISCCP calibration regression approach does not precisely determine the intercept
Pubs.GISS: Gornitz et al. 2020: Enhancing New York City's resilience to sea level rise and increased
https://www.giss.nasa.gov/pubs/abs/go05600n.html
findings, suffice for very high sea levels? Additional research is needed to determine technological, environmental, or economic
Pubs.GISS: Naud et al. 2018: Observational constraint for precipitation in extratropical cyclones: S
https://www.giss.nasa.gov/pubs/abs/na00400o.html
with GPM-CMB. A series of tests is conducted to determine the roles
Pubs.GISS: Naud et al. 2012: Using satellites to investigate the sensitivity of longwave downward ra
https://www.giss.nasa.gov/pubs/abs/na02200i.html
in-situ observations in these often remote locations are too sparse to determine the feedbacks
Pubs.GISS: Orbe et al. 2014: Seasonal ventilation of the stratosphere: Robust diagnostics from one-w
https://www.giss.nasa.gov/pubs/abs/or04100o.html
subject to fixed present-day climate forcings. From the one-way flux, we determine the mass
Pubs.GISS: Jansen et al. 2019: Climates of warm Earth-like planets II: Rotational 'Goldilocks' zones
https://www.giss.nasa.gov/pubs/abs/ja03300h.html
that of the modern Earth. By tracking precipitation and runoff we further determine that there is a
https://www.giss.nasa.gov/pubs/abs/ch03310d.html
for six tree species across 11 648 sites in Europe, to determine which were the
Pubs.GISS: Carter et al. 2024: Hyper illumination of exoplanets: Analytical and numerical approaches
https://www.giss.nasa.gov/pubs/abs/ca06030u.html
zone, penumbral zone, and unilluminated zone. The integrals required to determine the incident
https://www.giss.nasa.gov/pubs/abs/de03700v.html
to space; and the atmospheric processes that interacted with these to determine climate and habitability
Pubs.GISS: Wang et al. 1998: An empirical model study of the tropospheric meridional circulation bas
https://www.giss.nasa.gov/pubs/abs/wa04000r.html
the tropics. The obtained model vertical circulation is then used to determine the distribution
Pubs.GISS: Rind et al. 1973: Upper air wind speeds calculated from observations of natural infrasoun
https://www.giss.nasa.gov/pubs/abs/ri08200o.html
the sound speed based on temperature alone and the wind speed. We determine the former
https://www.giss.nasa.gov/pubs/abs/ka07200b.html
their simulated climate response, indicating that total AOD observations are far from sufficient to determine which model response is
Pubs.GISS: Stein and Walker 1965: Models of the upper atmosphere for a wide range of boundary condit
https://www.giss.nasa.gov/pubs/abs/st06010m.html
observations of satellite drag. They therefore demonstrate, quantitatively, that satellite drag data alone cannot determine atmospheric composition and
Pubs.GISS: Wu et al. 2015: Sensitivity of Intercalibration Uncertainty of the CLARREO Reflected Sola
https://www.giss.nasa.gov/pubs/abs/wu02100m.html
and spectral measurements from the SCIAMACHY instrument on Envisat are used to determine sensitivity of intercalibration