Joao Teixeira
Joao Teixeira
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Cited by
Cited by
Remote sensing of drought: Progress, challenges and opportunities
A AghaKouchak, A Farahmand, FS Melton, J Teixeira, MC Anderson, ...
Reviews of Geophysics 53 (2), 452-480, 2015
The representation of soil moisture freezing and its impact on the stable boundary layer
P Viterbo, A Beljaars, JF Mahfouf, J Teixeira
Quarterly Journal of the Royal Meteorological Society 125 (559), 2401-2426, 1999
Evaluation of cloud and water vapor simulations in CMIP5 climate models using NASA “A‐Train” satellite observations
JH Jiang, H Su, C Zhai, VS Perun, A Del Genio, LS Nazarenko, LJ Donner, ...
Journal of Geophysical Research: Atmospheres 117 (D14), 2012
A combined eddy-diffusivity mass-flux approach for the convective boundary layer
AP Siebesma, PMM Soares, J Teixeira
Journal of the atmospheric sciences 64 (4), 1230-1248, 2007
Entrainment and detrainment in cumulus convection: An overview
WC De Rooy, P Bechtold, K Fröhlich, C Hohenegger, H Jonker, ...
Quarterly Journal of the Royal Meteorological Society 139 (670), 1-19, 2013
Earth system modeling 2.0: A blueprint for models that learn from observations and targeted high‐resolution simulations
T Schneider, S Lan, A Stuart, J Teixeira
Geophysical Research Letters 44 (24), 12,396-12,417, 2017
An eddy‐diffusivity/mass‐flux parametrization for dry and shallow cumulus convection
PMM Soares, PMA Miranda, AP Siebesma, J Teixeira
Quarterly Journal of the Royal Meteorological Society: A journal of the …, 2004
Climate goals and computing the future of clouds
T Schneider, J Teixeira, CS Bretherton, F Brient, KG Pressel, C Schär, ...
Nature Climate Change 7 (1), 3-5, 2017
A planetary boundary layer height climatology derived from ECMWF reanalysis data
A von Engeln, J Teixeira
Journal of Climate 26 (17), 6575-6590, 2013
Navy operational global atmospheric prediction system (NOGAPS): Forcing for ocean models
TE Rosmond, J Teixeira, M Peng, TF Hogan, R Pauley
Oceanography 15 (1), 99-108, 2002
Tropical and subtropical cloud transitions in weather and climate prediction models: The GCSS/WGNE Pacific Cross-Section Intercomparison (GPCI)
J Teixeira, S Cardoso, M Bonazzola, J Cole, A DelGenio, C DeMott, ...
Journal of Climate 24 (20), 5223-5256, 2011
Time step sensitivity of nonlinear atmospheric models: numerical convergence, truncation error growth, and ensemble design
J Teixeira, CA Reynolds, K Judd
Journal of the atmospheric sciences 64 (1), 175-189, 2007
Stochastic nature of physical parameterizations in ensemble prediction: A stochastic convection approach
J Teixeira, CA Reynolds
Monthly Weather Review 136 (2), 483-496, 2008
A GCSS boundary-layer cloud model intercomparison study of the first ASTEX Lagrangian experiment
CS Bretherton, SK Krueger, MC Wyant, P Bechtold, E Van Meijgaard, ...
Boundary-Layer Meteorology 93, 341-380, 1999
Evaluating CMIP5 models using AIRS tropospheric air temperature and specific humidity climatology
B Tian, EJ Fetzer, BH Kahn, J Teixeira, E Manning, T Hearty
Journal of Geophysical Research: Atmospheres 118 (1), 114-134, 2013
A unified model for moist convective boundary layers based on a stochastic eddy-diffusivity/mass-flux parameterization
K Sušelj, J Teixeira, D Chung
Journal of the Atmospheric Sciences 70 (7), 1929-1953, 2013
An advection–diffusion scheme for the convective boundary layer: Description and 1D results
AP Siebesma, J Teixeira
Preprints, 14th Symp. on Boundary Layers and Turbulence, Aspen, CO, Amer …, 2000
Cloud representation in general‐circulation models over the northern Pacific Ocean: A EUROCS intercomparison study
AP Siebesma, C Jakob, G Lenderink, RAJ Neggers, J Teixeira, ...
Quarterly Journal of the Royal Meteorological Society: A journal of the …, 2004
Comparison of the ECMWF reanalysis with FIRE I observations: Diurnal variation of marine stratocumulus
PG Duynkerke, J Teixeira
Journal of climate 14 (7), 1466-1478, 2001
On the fidelity of large-eddy simulation of shallow precipitating cumulus convection
G Matheou, D Chung, L Nuijens, B Stevens, J Teixeira
Monthly Weather Review 139 (9), 2918-2939, 2011
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