1-28 of about 28 matches for site:www.giss.nasa.gov contribution agreement
https://www.giss.nasa.gov/pubs/abs/fr01000b.html
Pubs.GISS: Friedlingstein et al. 1995: On the contribution of CO 2 fertilization to the
Pubs.GISS: Bousquet et al. 2006: Contribution of anthropogenic and natural sources to atmospheric me
https://www.giss.nasa.gov/pubs/abs/bo04100j.html
Pubs.GISS: Bousquet et al. 2006: Contribution of anthropogenic and natural sources to
Pubs.GISS: Lee et al. 2023: Climate Change 2023: Synthesis Report. Contribution of Working Groups I,
https://www.giss.nasa.gov/pubs/abs/le06900s.html
GISS: Lee et al. 2023: Climate Change 2023: Synthesis Report. Contribution of Working Groups I, II and III
https://www.giss.nasa.gov/pubs/abs/ba08000d.html
models with and without a continuum contribution, and we find that none of the
Pubs.GISS: Boissoles et al. 2003: Theoretical calculation of the translation-rotation collision-indu
https://www.giss.nasa.gov/pubs/abs/bo08000d.html
element of the isotropic polarizability slightly, good agreement with experiment is obtained. For O 2 -O
https://www.giss.nasa.gov/pubs/abs/ar05100p.html
force has any effect on these quantities. The contribution to the unpolarized capture cross section for
https://www.giss.nasa.gov/pubs/abs/ba02000x.html
with several theoretical or empirical models, and satisfactory agreement is obtained with the models involving a
https://www.giss.nasa.gov/pubs/abs/ip02000c.html
In Climate Change 2013: The Physical Science Basis. Contribution of Working Group I to the
Pubs.GISS: Lowe et al. 1994: Climatic changes in areas adjacent to the North Atlantic during the las
https://www.giss.nasa.gov/pubs/abs/lo03100n.html
glacial-interglacial transition (14-9 ka BP): A contribution to IGCP-253. J. Quat. Sci. , 9 , no
Pubs.GISS: Houweling et al. 2000: The modeling of tropospheric methane: How well can point measureme
https://www.giss.nasa.gov/pubs/abs/ho02000x.html
sampling and the model, the agreement at situations as Bermuda East and Mace Head
https://www.giss.nasa.gov/pubs/abs/gr06900t.html
at the nuclei, unless the electronic contribution is nearly canceled by the nuclear contribution which is not the case for CIFmoments of CICN were in good agreement with Hartree-Fock (HF) calculations of McLean and
Pubs.GISS: Tegen and Miller 1998: A general circulation model study on the interannual variability o
https://www.giss.nasa.gov/pubs/abs/te04000r.html
satellite retrievals, and ground observations show mostly good agreement, but also reveal problems with the model results
https://www.giss.nasa.gov/pubs/abs/st02600e.html
intermediate to high mass that show remarkably close agreement with observed stars, under otherwise standard physical assumptions. Most or
https://www.giss.nasa.gov/pubs/abs/go01000b.html
that predict a zero to negative contribution to SLR from Antarctica. Most global climate models
https://www.giss.nasa.gov/pubs/abs/ca03220j.html
to the general formula, which involves the contribution of the whole spectrum of the
Pubs.GISS: Heck 1977: A comparison of estimated and directly measured turbulent heat fluxes in the l
https://www.giss.nasa.gov/pubs/abs/he00200p.html
105<1337:ACOEAD>2.0.CO;2. The contribution of small-scale motions to the
https://www.giss.nasa.gov/pubs/abs/ko08000d.html
the free troposphere in polluted regions. Model agreement with surface observations is not remarkably different from previous studies
Pubs.GISS: D'Arrigo 1989: Dendrochronological Modeling and Reconstruction of Large-Scale Climate Var
https://www.giss.nasa.gov/pubs/abs/da00100w.html
completely explained by past climate-growth relationships. The contribution of atmosphere-biosphere CO 2 exchange of
Pubs.GISS: Boissoles et al. 2005: New experimental measurements and theoretical analysis of the coll
https://www.giss.nasa.gov/pubs/abs/bo01100t.html
at low enough pressures so that the binary contribution is dominant. Previous measurements have been made at pressures where
Pubs.GISS: Li et al. 2010: An optimal fitting approach to improve the GISS ModelE aerosol optical pr
https://www.giss.nasa.gov/pubs/abs/li00500s.html
adjusting the aerosol's dry size, the agreement between the GCM AE with AERONET data is
https://www.giss.nasa.gov/pubs/abs/tr05100g.html
properties of nuclei. Assuming that the contribution to the cross section of a
Pubs.GISS: Smit et al. 2019: In-flight validation of SPEX airborne spectro-polarimeter onboard NASA'
https://www.giss.nasa.gov/pubs/abs/sm01200v.html
climate and air quality studies. In this contribution, we provide an detailed description of the multi
https://www.giss.nasa.gov/pubs/abs/ca04720o.html
1175/JPO-D-19-0043.1. The mesoscale contribution to subduction in the Southern
https://www.giss.nasa.gov/pubs/abs/ho04700w.html
Center for Climate Systems Research. The agreement signed in Paris in 2015 is
Pubs.GISS: Kageyama et al. 2021: A multi-model CMIP6-PMIP4 study of Arctic sea ice at 127 ka: Sea ic
https://www.giss.nasa.gov/pubs/abs/ka01400p.html
the Paleoclimate Modelling Intercomparison Project for its contribution to the sixth phase of the
https://www.giss.nasa.gov/research/briefs/2021_rosenzweig_07/
in efforts to achieve the Paris Agreement goals. Notably, the research finds that the
https://www.giss.nasa.gov/pubs/authors/gschmidt.html
Schmidt , 2022: Assessing progress toward the Paris Climate Agreement from space . Environ. Res. Lett. , 17 , no. 11, 111002, doi
https://www.giss.nasa.gov/pubs/authors/ktsigaridis.html
forcing differences and initial conditions on inter-model agreement in the VolMIP volc-pinatubo-full experiment