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1-65 of about 65 matches for site:pubs.giss.nasa.gov abs regime
https://pubs.giss.nasa.gov/abs/ch03010w.html
Pubs.GISS: Chen et al. 2011: Projected regime shift in Arctic cloud and water vapor feedbacks Go
https://pubs.giss.nasa.gov/abs/mc07100r.html
Pubs.GISS: McCoy et al. 2020: A regime-oriented approach to observationally constraining extratropical shortwave... Go to
https://pubs.giss.nasa.gov/abs/mi02310d.html
Pubs.GISS: Miller et al. 2007: Future regime shift in feedbacks during Arctic winter Go to Main
https://pubs.giss.nasa.gov/abs/re08000i.html
Pubs.GISS: Rémillard and Tselioudis 2015: Cloud regime variability over the Azores and its application
https://pubs.giss.nasa.gov/abs/pa03500b.html
Pubs.GISS: Parham et al. 2011: Astronomical tidal regime change as a control on the Holocene development
https://pubs.giss.nasa.gov/abs/su03100m.html
Pubs.GISS: Su et al. 2013: Diagnosis of regime-dependent cloud simulation errors in CMIP5 models using
https://pubs.giss.nasa.gov/abs/to07200b.html
al. 2023: On the impact of a dry intrusion driving cloud-regime transitions in a
https://pubs.giss.nasa.gov/abs/ta05200z.html
novel "double decomposition method" that employs the "cloud radiative kernel" and "cloud regime" concepts, to two
https://pubs.giss.nasa.gov/abs/ro02800o.html
particular, the Northern Hemisphere (NH) subtropics undergo a change in dynamic regime during the local
https://pubs.giss.nasa.gov/abs/de09700b.html
widespread. The most slowly rotating, most highly irradiated planets, though, occupy a hydrological regime unlike any on Earth
https://pubs.giss.nasa.gov/abs/de09600r.html
gas concentrations do not necessarily produce more open ocean area because of possible dynamic regime transitions. For an
https://pubs.giss.nasa.gov/abs/pa05700x.html
on the atmospheric boundary layer is described by means of a regime classification based on Self
https://pubs.giss.nasa.gov/abs/ca05400j.html
since Ri l (cr) determines the upper limit of a laminar regime (superscript l), it has
https://pubs.giss.nasa.gov/abs/ca01200l.html
so strong that it suppresses the energy cascade process and no inertial regime can develop. In
https://pubs.giss.nasa.gov/abs/or05200z.html
the North Atlantic circulation under a mid-range future climate scenario: A regime shift in Northern
https://pubs.giss.nasa.gov/abs/to06200a.html
with satellite-observed trends in droplet number concentration upwind of CAO cloud-regime transitions over the
https://pubs.giss.nasa.gov/abs/ch09800r.html
I). In this study, it is shown that one of several PDV interdecadal regime shifts occurred during the
https://pubs.giss.nasa.gov/abs/ca05900x.html
3, in accord with recent data; (2) in the inertial-conductive regime, the model
https://pubs.giss.nasa.gov/abs/ca04710r.html
In the ocean, there are two main regimes where non-local transport is important. One regime is where storms release
https://pubs.giss.nasa.gov/abs/ca04720o.html
2011 (SR11) using the following mesoscale model. The adiabatic (A) regime was modeled with the
https://pubs.giss.nasa.gov/abs/ja03300h.html
a planet's surface that falls in the 0 ≤ T ≤ 100°C temperature regime, we find a
https://pubs.giss.nasa.gov/abs/qu07000h.html
it was decided that ACPC would pursue separate studies for a shallow cloud regime and a
https://pubs.giss.nasa.gov/abs/we07300l.html
the planet was dominated by higher mantle temperatures (by about 200°C), an uncertain tectonic regime that likely included squishy
https://pubs.giss.nasa.gov/abs/cr02100m.html
subset of latest climate models participating in CMIP6. We strive for regime-oriented model validation and
https://pubs.giss.nasa.gov/abs/co07500u.html
precipitation and shifts the region to a drier evaporative regime, leading to a
https://pubs.giss.nasa.gov/abs/mc04100o.html
such as the strength of land-atmosphere coupling and evaporative regime. We conduct sensitivity experiments
https://pubs.giss.nasa.gov/abs/ji07300l.html
drought is severe enough to cause a shift from an energy-limited regime to a
https://pubs.giss.nasa.gov/abs/ja05100g.html
climatic change that involves crossing a threshold to a new climate regime (e.g., new mean state
https://pubs.giss.nasa.gov/abs/al04500b.html
our analysis were not large enough to observe the boundedness-induced asymptotic regime in AOT
https://pubs.giss.nasa.gov/abs/ri00200p.html
that the stratospheric response is very individualistic to the particular climate regime, and the
https://pubs.giss.nasa.gov/abs/ma02300a.html
GCM. The realistic depiction of evaporation also affects the thermal regime in the
https://pubs.giss.nasa.gov/abs/ca05710o.html
two arguments most frequently cited to neglect Σ: (1) in an adiabatic regime, fluxes across isopycnal surfaces
https://pubs.giss.nasa.gov/abs/de00500s.html
Forest Fire Behavior Prediction (FBP) System, to local vegetation, climate, and fire regime conditions. A smoke
https://pubs.giss.nasa.gov/abs/al07000g.html
off not only for large particle sizes but also in small particles regime which prevents the
https://pubs.giss.nasa.gov/abs/va03300h.html
and atmospheric models with a better representation of the complex fire regime in this
https://pubs.giss.nasa.gov/abs/pe03100m.html
the Holocene warming appears to be greater than that generated by an equivalent insolation regime 80 ka. A
https://pubs.giss.nasa.gov/abs/ji00100k.html
reduce the capacity for carbon sequestration as RDOC. The nutrient regime enabling maximum carbon storage
https://pubs.giss.nasa.gov/abs/ca08320k.html
that the presence of vorticity in a stably stratified regime, such as the
https://pubs.giss.nasa.gov/abs/fr09200d.html
properties in the 20 May case are similar to a tropical regime, likely associated with warm
https://pubs.giss.nasa.gov/abs/mi00220m.html
and the favored assumption was found to be sensitive to cloud regime (cumuliform/stratiform). Confirming previous
https://pubs.giss.nasa.gov/abs/ka07300l.html
and radius sensitivity of exoplanet discovery capabilities has reached into the terrestrial regime. The focus
https://pubs.giss.nasa.gov/abs/ri00800v.html
opportunity to assess how atmospheric circulation changes when in a different climate regime, one characterized by much
https://pubs.giss.nasa.gov/abs/ot08000d.html
is shown that the glint properties are governed mainly by the capillary regime. Get PDF (3.5
https://pubs.giss.nasa.gov/abs/ha04510h.html
regimes. The regimes associated with cyclones have the highest in-regime shortwave cloud radiative effect
https://pubs.giss.nasa.gov/abs/pu07000g.html
a weak influence on total evapotranspiration, and a negligible impact on runoff. Climate regime and characteristic
https://pubs.giss.nasa.gov/abs/ye01000b.html
to a warmer and colder climate: In a warmer regime moist convection determines the
https://pubs.giss.nasa.gov/abs/he02000x.html
ice sheet in the continental interior, whereas under the current climatic regime beginning in the
https://pubs.giss.nasa.gov/abs/ot00100w.html
and cirrus optical depth, which was found in the subvisual/threshold-visible regime, confirming the utility
https://pubs.giss.nasa.gov/abs/tu08100v.html
through the barrier. Several newly discovered quantum effects become possible in this regime, including power amplification of
https://pubs.giss.nasa.gov/abs/ca04320y.html
Southern Ocean, where there is the largest CO 2 absorption, the dominant regime is diffusive convection discussed
https://pubs.giss.nasa.gov/abs/ce07200b.html
to Sc. Decomposition of the bias reveals that the Sc-regime cloud fraction is better
https://pubs.giss.nasa.gov/abs/du03100n.html
1 (WS1) deep convection cloud state and an independent, microwave-based deep convective precipitation regime developed here. The
https://pubs.giss.nasa.gov/abs/ca04620e.html
on the ratio h/H, where h is depth of the SM regime and H
https://pubs.giss.nasa.gov/abs/ba03800f.html
to have been ∼20° per Earth day. To investigate the dynamical regime of this
https://pubs.giss.nasa.gov/abs/ca01620b.html
The resulting vertical velocity depends on the extent of the SM regime, the horizontal
https://pubs.giss.nasa.gov/abs/ku03100m.html
the tropical atmosphere. This study examines the evolution of the hydrologic regime from before the
https://pubs.giss.nasa.gov/abs/ro02810a.html
thermodynamics contribute to the inadequate simulation of the low-concentration regime in many
https://pubs.giss.nasa.gov/abs/mc06100q.html
and aerosol to cloud. Here, we restrict our analysis to the regime of extratropical
https://pubs.giss.nasa.gov/abs/ka08300m.html
to exoplanet demographics that can be placed in the potential runaway greenhouse regime where Venus analogs are
https://pubs.giss.nasa.gov/abs/wa08700a.html
the other a fully coupled dynamic bathtub type ocean. The dynamical regime transitions that occur as
https://pubs.giss.nasa.gov/abs/ne00100k.html
layer schemes for weather and climate models for this cloud regime, using large-eddy simulations
https://pubs.giss.nasa.gov/abs/ca01300e.html
of the scaling variable Ra/Ra * ; this corresponds to the first regime. For Ra
https://pubs.giss.nasa.gov/abs/ca01400w.html
lies the fact that we are dealing with a highly nonlinear, turbulent regime under the action
https://pubs.giss.nasa.gov/abs/fa09000j.html
and they can be considered to be in an eddy saturated regime. Larger contrasts arise when
https://pubs.giss.nasa.gov/abs/ca09220p.html
model reproduces. Heat to salt flux ratio. In the Ri ≫ 1 regime, the RSM