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Artykuły w czasopismach na temat „Moist dynamics”

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Data publikacji: 6 września 2023

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1

JIANG, QINGFANG. "Moist dynamics and orographic precipitation." Tellus A 55, no. 4 (2003): 301–16. http://dx.doi.org/10.1034/j.1600-0870.2003.00025.x.

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2

Jiang, Qingfang. "Moist dynamics and orographic precipitation." Tellus A: Dynamic Meteorology and Oceanography 55, no. 4 (2003): 301–16. http://dx.doi.org/10.3402/tellusa.v55i4.14577.

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Palotai, Csaba, Shawn Brueshaber, Ramanakumar Sankar, and Kunio Sayanagi. "Moist Convection in the Giant Planet Atmospheres." Remote Sensing 15, no. 1 (2022): 219. http://dx.doi.org/10.3390/rs15010219.

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The outer planets of our Solar System display a myriad of interesting cloud features, of different colors and sizes. The differences between the types of observed clouds suggest a complex interplay between the dynamics and chemistry at play in these atmospheres. Particularly, the stark difference between the banded structures of Jupiter and Saturn vs. the sporadic clouds on the ice giants highlights the varieties in dynamic, chemical and thermal processes that shape these atmospheres. Since the early explorations of these planets by spacecrafts, such as Voyager and Voyager 2, there are many ou

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4

Hunter, Maria O., Michael Keller, Douglas Morton, et al. "Structural Dynamics of Tropical Moist Forest Gaps." PLOS ONE 10, no. 7 (2015): e0132144. http://dx.doi.org/10.1371/journal.pone.0132144.

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MAJDA, ANDREW J., YULONG XING, and MAJID MOHAMMADIAN. "Moist multi-scale models for the hurricane embryo." Journal of Fluid Mechanics 657 (June 30, 2010): 478–501. http://dx.doi.org/10.1017/s0022112010001515.

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Determining the finite-amplitude preconditioned states in the hurricane embryo, which lead to tropical cyclogenesis, is a central issue in contemporary meteorology. In the embryo there is competition between different preconditioning mechanisms involving hydrodynamics and moist thermodynamics, which can lead to cyclogenesis. Here systematic asymptotic methods from applied mathematics are utilized to develop new simplified moist multi-scale models starting from the moist anelastic equations. Three interesting multi-scale models emerge in the analysis. The balanced mesoscale vortex (BMV) dynamic

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6

Prasanna, V., and H. Annamalai. "Moist Dynamics of Extended Monsoon Breaks over South Asia." Journal of Climate 25, no. 11 (2012): 3810–31. http://dx.doi.org/10.1175/jcli-d-11-00459.1.

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In the present research to identify moist processes that initiate and maintain extended monsoon breaks over South Asia moisture and moist static energy (MSE) budgets are performed on the newly available European Centre for Medium-Range Weather Forecasts Interim reanalysis (ERA-Interim) and ensemble integrations from a coupled model. The hypothesis that interaction between moist physics and regional circulation and the role of cloud–radiation feedbacks are important is tested. Budget diagnostics show that dry advection is the principal moist process to initiate extended breaks. Its sources are

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7

Straus, David M., and Mary Ann Huntley. "Interactions between Moist Heating and Dynamics in Atmospheric Predictability." Journal of the Atmospheric Sciences 51, no. 3 (1994): 447–64. http://dx.doi.org/10.1175/1520-0469(1994)051<0447:ibmhad>2.0.co;2.

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8

Biello, Joseph A., and Andrew J. Majda. "Intraseasonal multi-scale moist dynamics of the tropical atmosphere." Communications in Mathematical Sciences 8, no. 2 (2010): 519–40. http://dx.doi.org/10.4310/cms.2010.v8.n2.a11.

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9

Thatcher, Diana R., and Christiane Jablonowski. "A moist aquaplanet variant of the Held–Suarez test for atmospheric model dynamical cores." Geoscientific Model Development 9, no. 4 (2016): 1263–92. http://dx.doi.org/10.5194/gmd-9-1263-2016.

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Abstract. A moist idealized test case (MITC) for atmospheric model dynamical cores is presented. The MITC is based on the Held–Suarez (HS) test that was developed for dry simulations on “a flat Earth” and replaces the full physical parameterization package with a Newtonian temperature relaxation and Rayleigh damping of the low-level winds. This new variant of the HS test includes moisture and thereby sheds light on the nonlinear dynamics–physics moisture feedbacks without the complexity of full-physics parameterization packages. In particular, it adds simplified moist processes to the HS forci

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10

Thatcher, D. R., and C. Jablonowski. "A moist aquaplanet variant of the Held–Suarez test for atmospheric model dynamical cores." Geoscientific Model Development Discussions 8, no. 9 (2015): 8263–340. http://dx.doi.org/10.5194/gmdd-8-8263-2015.

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Abstract. A moist idealized test case (MITC) for atmospheric model dynamical cores is presented. The MITC is based on the Held–Suarez (HS) test that was developed for dry simulations on a flat Earth and replaces the full physical parameterization package with a Newtonian temperature relaxation and Rayleigh damping of the low-level winds. This new variant of the HS test includes moisture and thereby sheds light on the non-linear dynamics-physics moisture feedbacks without the complexity of full physics parameterization packages. In particular, it adds simplified moist processes to the HS forcin

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11

Nie, Ji, Panxi Dai, and Adam H. Sobel. "Dry and moist dynamics shape regional patterns of extreme precipitation sensitivity." Proceedings of the National Academy of Sciences 117, no. 16 (2020): 8757–63. http://dx.doi.org/10.1073/pnas.1913584117.

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Responses of extreme precipitation to global warming are of great importance to society and ecosystems. Although observations and climate projections indicate a general intensification of extreme precipitation with warming on global scale, there are significant variations on the regional scale, mainly due to changes in the vertical motion associated with extreme precipitation. Here, we apply quasigeostrophic diagnostics on climate-model simulations to understand the changes in vertical motion, quantifying the roles of dry (large-scale adiabatic flow) and moist (small-scale convection) dynamics

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12

Smith, Samuel, Paul W. Staten, and Jian Lu. "How Moist and Dry Intrusions Control the Local Hydrologic Cycle in Present and Future Climates." Journal of Climate 34, no. 11 (2021): 4343–59. http://dx.doi.org/10.1175/jcli-d-20-0780.1.

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AbstractModels disagree on how much the hydrologic cycle could intensify under climate change. These changes are expected to scale with the Clausius–Clapeyron relation but may locally diverge due in part to the uncertain response of the general circulation, causing the hydrologic cycle to inherit this uncertainty. To identify how the circulation contributes, we link circulation changes to changes in the higher moments of the hydrologic cycle using the novel dynamical framework of the local hydrologic cycle, the portion of the hydrologic cycle driven by moist or dry intrusions. We expand this d

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13

Castelli, Fabio, Rafael L. Bras, and Kerry A. Emanuel. "An Analytical Approach to the Nonlinear Dynamics of Moist Frontogenesis." Journal of the Atmospheric Sciences 50, no. 11 (1993): 1504–18. http://dx.doi.org/10.1175/1520-0469(1993)050<1504:aaattn>2.0.co;2.

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14

Kurowski, Marcin J., Wojciech W. Grabowski, and Piotr K. Smolarkiewicz. "Anelastic and Compressible Simulation of Moist Dynamics at Planetary Scales." Journal of the Atmospheric Sciences 72, no. 10 (2015): 3975–95. http://dx.doi.org/10.1175/jas-d-15-0107.1.

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Abstract Moist anelastic and compressible numerical solutions to the planetary baroclinic instability and climate benchmarks are compared. The solutions are obtained by applying a consistent numerical framework for discrete integrations of the various nonhydrostatic flow equations. Moist extension of the baroclinic instability benchmark is formulated as an analog of the dry case. Flow patterns, surface vertical vorticity and pressure, total kinetic energy, power spectra, and total amount of condensed water are analyzed. The climate benchmark extends the baroclinic instability study by addressi

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15

Chan, Douglas, and Han‐Ru Cho. "The dynamics of moist frontogenesis in a semi‐geostrophic model." Atmosphere-Ocean 29, no. 1 (1991): 85–101. http://dx.doi.org/10.1080/07055900.1991.9649394.

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16

Kravtsov, Sergey, Ilijana Mastilovic, Andrew McC Hogg, William K. Dewar, and Jeffrey R. Blundell. "The Moist Quasi-Geostrophic Coupled Model: MQ-GCM 2.0." Geoscientific Model Development 15, no. 19 (2022): 7449–69. http://dx.doi.org/10.5194/gmd-15-7449-2022.

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Abstract. This paper contains a description of recent changes to the formulation and numerical implementation of the Quasi-Geostrophic Coupled Model (Q-GCM), which constitute a major update of the previous version of the model (Hogg et al., 2014). The Q-GCM model has been designed to provide an efficient numerical tool to study the dynamics of multi-scale midlatitude air–sea interactions and their climatic impacts. The present additions/alterations were motivated by an inquiry into the dynamics of mesoscale ocean–atmosphere coupling and, in particular, by an apparent lack of the Q-GCM atmosphe

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17

Zhang, Yi, Jian Li, Rucong Yu, et al. "A Multiscale Dynamical Model in a Dry-Mass Coordinate for Weather and Climate Modeling: Moist Dynamics and Its Coupling to Physics." Monthly Weather Review 148, no. 7 (2020): 2671–99. http://dx.doi.org/10.1175/mwr-d-19-0305.1.

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Abstract A multiscale dynamical model for weather forecasting and climate modeling is developed and evaluated in this study. It extends a previously established layer-averaged, unstructured-mesh nonhydrostatic dynamical core (dycore) to moist dynamics and parameterized physics in a dry-mass vertical coordinate. The dycore and tracer transport components are coupled in a mass-consistent manner, with the dycore providing time-averaged horizontal mass fluxes to passive transport, and tracer transport feeding back to the dycore with updated moisture constraints. The vertical mass flux in the trace

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18

Kurowski, Marcin J., Wojciech W. Grabowski, and Piotr K. Smolarkiewicz. "Anelastic and Compressible Simulation of Moist Deep Convection." Journal of the Atmospheric Sciences 71, no. 10 (2014): 3767–87. http://dx.doi.org/10.1175/jas-d-14-0017.1.

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Abstract Anelastic and compressible solutions are compared for two moist deep convection benchmarks, a two-dimensional thermal rising in a saturated moist-neutral deep atmosphere, and a three-dimensional supercell formation. In the anelastic model, the pressure applied in the moist thermodynamics comes from either the environmental hydrostatically balanced pressure profile in the standard anelastic model or is combined with nonhydrostatic perturbations from the elliptic pressure solver in the generalized anelastic model. The compressible model applies either an explicit acoustic-mode-resolving

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19

Fuhrer, Oliver, and Christoph Schär. "Dynamics of Orographically Triggered Banded Convection in Sheared Moist Orographic Flows." Journal of the Atmospheric Sciences 64, no. 10 (2007): 3542–61. http://dx.doi.org/10.1175/jas4024.1.

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Abstract Shallow orographic convection embedded in an unstable cap cloud can organize into convective bands. Previous research has highlighted the important role of small-amplitude topographic variations in triggering and organizing banded convection. Here, the underlying dynamical mechanisms are systematically investigated by conducting three-dimensional simulations of moist flows past a two-dimensional mountain ridge using a cloud-resolving numerical model. Most simulations address a sheared environment to account for the observed wind profiles. Results confirm that small-amplitude topograph

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20

Arnolds, E. "Dynamics of macrofungi in two moist heathlands in Drenthe, The Netherlands." Acta Botanica Neerlandica 37, no. 2 (1988): 291–305. http://dx.doi.org/10.1111/j.1438-8677.1988.tb02137.x.

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21

Deremble, Bruno, Guillaume Lapeyre, and Michael Ghil. "Atmospheric Dynamics Triggered by an Oceanic SST Front in a Moist Quasigeostrophic Model." Journal of the Atmospheric Sciences 69, no. 5 (2012): 1617–32. http://dx.doi.org/10.1175/jas-d-11-0288.1.

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Abstract To understand the atmospheric response to a midlatitude oceanic front, this paper uses a quasigeostrophic (QG) model with moist processes. A well-known, three-level QG model on the sphere has been modified to include such processes in an aquaplanet setting. Its response is analyzed in terms of the upper-level atmospheric jet for sea surface temperature (SST) fronts of different profiles and located at different latitudes. When the SST front is sufficiently strong, it tends to anchor the mean atmospheric jet, suggesting that the jet’s spatial location and pattern are mainly affected by

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22

Fuhrer, Oliver, and Christoph Schär. "Embedded Cellular Convection in Moist Flow past Topography." Journal of the Atmospheric Sciences 62, no. 8 (2005): 2810–28. http://dx.doi.org/10.1175/jas3512.1.

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Abstract Marginally unstable air masses impinging upon a mountain ridge may lead to the development of a nominally stratiform orographic cloud with shallow embedded convection. Rainfall amounts and distribution are then strongly influenced by the convective dynamics. In this study, the transition from purely stratiform orographic precipitation to flow regimes with embedded convection is systematically investigated. To this end, idealized cloud-resolving numerical simulations of moist flow past a two-dimensional mountain ridge are performed in a three-dimensional domain. A series of simulations

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23

Joshi, Prakash C., Jeffrey A. Lockwood, N. Vashishth, and A. Singh. "Grasshopper (Orthoptera: Acridoidea) Community Dynamics in a Moist Deciduous Forest in India." Journal of Orthoptera Research, no. 8 (November 1999): 17. http://dx.doi.org/10.2307/3503420.

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24

Wang, Bin, та Hualan Rui. "Dynamics of the Coupled Moist Kelvin–Rossby Wave on an Equatorialβ-Plane". Journal of the Atmospheric Sciences 47, № 4 (1990): 397–413. http://dx.doi.org/10.1175/1520-0469(1990)047<0397:dotcmk>2.0.co;2.

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25

Bishop, Craig H., and Alan J. Thorpe. "Frontal Wave Stability during Moist Deformation Frontogenesis. Part I: Linear Wave Dynamics." Journal of the Atmospheric Sciences 51, no. 6 (1994): 852–73. http://dx.doi.org/10.1175/1520-0469(1994)051<0852:fwsdmd>2.0.co;2.

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26

Dalling, J. W., M. D. Swaine, and Nancy C. Garwood. "Soil seed bank community dynamics in seasonally moist lowland tropical forest, Panama." Journal of Tropical Ecology 13, no. 5 (1997): 659–80. http://dx.doi.org/10.1017/s0266467400010853.

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ABSTRACTSeasonal changes in the densities of dormant seeds in the soil around eight pioneer trees in the 50-ha Forest Dynamics Plot, on Barro Colorado Island, Panamá were studied, and how seed dispersal and seed dormancy influenced patterns of seed abundance and distribution were examined. Twenty-four, 3-cm-deep soil samples were collected on 30 m transects radiating out from each of the trees in each of four time-intervals through the year, and four 21-cm-deep samples were collected beneath the focal tree crowns. In the surface 0–3 cm of soil, germinable seed densities of all species combined

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27

Valappil, Narayanan I., and K. Swarupanandan. "Regeneration dynamics and sylvigenesis in the moist deciduous forests of southwest India." New Forests 11, no. 3 (1996): 185–205. http://dx.doi.org/10.1007/bf00036782.

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28

Kurowski, Marcin J., Wojciech W. Grabowski, and Piotr K. Smolarkiewicz. "Toward Multiscale Simulation of Moist Flows with Soundproof Equations." Journal of the Atmospheric Sciences 70, no. 12 (2013): 3995–4011. http://dx.doi.org/10.1175/jas-d-13-024.1.

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Abstract This paper discusses the incorporation of phase changes of the water substance that accompany moist atmospheric flows into the all-scale atmospheric model based on soundproof equations. A specific issue involves developing a theoretical basis and practical implementation to include pressure perturbations associated with atmospheric circulations, from small scale to global, into representations of moist thermodynamics. In small-scale modeling using soundproof equations, pressure perturbations are obtained from the elliptic pressure solver and are typically excluded from the moist therm

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29

Conzemius, Robert J., Richard W. Moore, Michael T. Montgomery, and Christopher A. Davis. "Mesoscale Convective Vortex Formation in a Weakly Sheared Moist Neutral Environment." Journal of the Atmospheric Sciences 64, no. 5 (2007): 1443–66. http://dx.doi.org/10.1175/jas3898.1.

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Abstract Idealized simulations of a diabatic Rossby vortex (DRV) in an initially moist neutral baroclinic environment are performed using the fifth-generation National Center for Atmospheric Research–Pennsylvania State University (NCAR–PSU) Mesoscale Model (MM5). The primary objective is to test the hypothesis that the formation and maintenance of midlatitude warm-season mesoscale convective vortices (MCVs) are largely influenced by balanced flow dynamics associated with a vortex that interacts with weak vertical shear. As a part of this objective, the simulated DRV is placed within the contex

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30

O’Gorman, Paul A. "The Effective Static Stability Experienced by Eddies in a Moist Atmosphere." Journal of the Atmospheric Sciences 68, no. 1 (2011): 75–90. http://dx.doi.org/10.1175/2010jas3537.1.

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Abstract Water vapor directly affects the dynamics of atmospheric eddy circulations through the release of latent heat. But it is difficult to include latent heat release in dynamical theories because of the associated nonlinearity (precipitation generally occurs where there is upward motion). A new effective static stability is derived that fundamentally captures the effect of latent heat release on moist eddy circulations. It differs from the usual dry static stability by an additive term that depends on temperature and a parameter measuring the up–down asymmetry of vertical velocity statist

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31

Morrison, Hugh, and John M. Peters. "Theoretical Expressions for the Ascent Rate of Moist Deep Convective Thermals." Journal of the Atmospheric Sciences 75, no. 5 (2018): 1699–719. http://dx.doi.org/10.1175/jas-d-17-0295.1.

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An approximate analytic expression is derived for the ratio λ of the ascent rate of moist deep convective thermals and the maximum vertical velocity within them; λ is characterized as a function of two nondimensional buoyancy-dependent parameters y and h and is used to express the thermal ascent rate as a function of the buoyancy field. The parameter y characterizes the vertical distribution of buoyancy within the thermal, and h is the ratio of the vertically integrated buoyancy from the surface to the thermal top and the vertical integral of buoyancy within the thermal. Theoretical λ values a

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32

Demoz, Belay B., Ruben Delgado, Brian Caroll, et al. "Lidar Profiling In the lower Troposphere: experience from PECAN." EPJ Web of Conferences 176 (2018): 10004. http://dx.doi.org/10.1051/epjconf/201817610004.

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Results from the PECAN (Plains Elevated Convection at Night) campaign are discussed. In particular, the utility of simple backscatter lidars/ceilometers in quantifying atmospheric dynamics parameters and variables as well as evolution of the lower tropospheric dynamics are made. Cases of bore wave dynamics and the potential of these events in lofting of low level, moist, airmass and its consequence in thunderstorm initiation are made. A suite of thermodynamic profiling instruments are combined and compared to describe and visualize lower tropospheric dynamic evolution.

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33

Zhang, Fuqing, Naifang Bei, Richard Rotunno, Chris Snyder, and Craig C. Epifanio. "Mesoscale Predictability of Moist Baroclinic Waves: Convection-Permitting Experiments and Multistage Error Growth Dynamics." Journal of the Atmospheric Sciences 64, no. 10 (2007): 3579–94. http://dx.doi.org/10.1175/jas4028.1.

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Abstract A recent study examined the predictability of an idealized baroclinic wave amplifying in a conditionally unstable atmosphere through numerical simulations with parameterized moist convection. It was demonstrated that with the effect of moisture included, the error starting from small random noise is characterized by upscale growth in the short-term (0–36 h) forecast of a growing synoptic-scale disturbance. The current study seeks to explore further the mesoscale error-growth dynamics in idealized moist baroclinic waves through convection-permitting experiments with model grid incremen

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34

Sumi, Yukari, and Hirohiko Masunaga. "A Moist Static Energy Budget Analysis of Quasi-2-Day Waves Using Satellite and Reanalysis Data." Journal of the Atmospheric Sciences 73, no. 2 (2016): 743–59. http://dx.doi.org/10.1175/jas-d-15-0098.1.

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Abstract A moist static energy (MSE) budget analysis is applied to quasi-2-day waves to examine the effects of thermodynamic processes on the wave propagation mechanism. The 2-day waves are defined as westward inertia–gravity (WIG) modes identified with filtered geostationary infrared measurements, and the thermodynamic parameters and MSE budget variables computed from reanalysis data are composited with respect to the WIG peaks. The composite horizontal and vertical MSE structures are overall as theoretically expected from WIG wave dynamics. A prominent horizontal MSE advection is found to ex

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35

Yamada, Ray, and Olivier Pauluis. "Momentum Balance and Eliassen–Palm Flux on Moist Isentropic Surfaces." Journal of the Atmospheric Sciences 73, no. 3 (2016): 1293–314. http://dx.doi.org/10.1175/jas-d-15-0229.1.

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Abstract Previous formulations for the zonally averaged momentum budget and Eliassen–Palm (EP) flux diagnostics do not adequately account for moist dynamics, since air parcels are not differentiated by their moisture content when averages are taken. The difficulty in formulating the momentum budget in moist coordinates lies in the fact that they are generally not invertible with height. Here, a conditional-averaging approach is used to derive a weak formulation of the momentum budget and EP flux in terms of a general vertical coordinate that is not assumed to be invertible. The generalized equ

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36

Atamanyuk, Volodymyr, and Yaroslav Gumnytskyi. "Mass Exchange Dynamics During the Second Filtration Drying Period." Chemistry & Chemical Technology 3, no. 2 (2009): 129–37. http://dx.doi.org/10.23939/chcht03.02.129.

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The work is dedicated to theoretical and experimental investigations of kinetics and dynamics of filtration drying of capillary and pore materials, and mineral granulated fertilizers, in particular. The proposed physical model of a moist particle and the differential system of equations which describes heat exchange in the second drying period enables to determine the transfer velocity of mass-exchange zone in a dispersion layer of the material during filtration drying.

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37

Talemos, Seta, Demissew Sebsebe, and Woldu Zerihun. "Litterfall dynamics in Boter-Becho Forest: Moist evergreen montane forest of Southwestern Ethiopia." Journal of Ecology and The Natural Environment 10, no. 1 (2018): 13–21. http://dx.doi.org/10.5897/jene2017.0648.

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Gautam, Tilak Prasad, and Tej Narayan Mandal. "Effect of disturbance on litter dynamics in moist tropical forest of eastern Nepal." Our Nature 14, no. 1 (2017): 1–12. http://dx.doi.org/10.3126/on.v14i1.16435.

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Litterfall is an important vector of nutrient and carbon recycling in forest ecosystems. Present study was conducted in moist tropical forest of eastern Nepal to understand the effect of disturbance on litter dynamics. Litterfall was estimated at monthly intervals from one litter trap (1 m × 1 m) at each of the 70 sampling plots while litter mass accumulated at each sampling plot was collected once every season from one 1 m × 1 m plot. The total annual litterfall in undisturbed forest (UF) was 11.8 Mg ha−1 yr−1 which decreased by 54.2% in disturbed forest (DF). Leaves accounted for 69% (UF) to

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39

You, Bo. "Dynamics of the three dimensional viscous primitive equations of large-scale moist atmosphere." Communications in Mathematical Sciences 19, no. 6 (2021): 1673–701. http://dx.doi.org/10.4310/cms.2021.v19.n6.a10.

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Dalling, J. W., M. D. Swaine, and Nancy C. Garwood. "DISPERSAL PATTERNS AND SEED BANK DYNAMICS OF PIONEER TREES IN MOIST TROPICAL FOREST." Ecology 79, no. 2 (1998): 564–78. http://dx.doi.org/10.1890/0012-9658(1998)079[0564:dpasbd]2.0.co;2.

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Pillai, Prasanth A., and H. Annamalai. "Moist Dynamics of Severe Monsoons over South Asia: Role of the Tropical SST*." Journal of the Atmospheric Sciences 69, no. 1 (2012): 97–115. http://dx.doi.org/10.1175/jas-d-11-056.1.

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Abstract Diagnostics from observations and multicentury integrations of a coupled model [Geophysical Fluid Dynamics Laboratory (GFDL) coupled model version 2.1 (CM2.1)] indicate that about 65% of the severe monsoons (rainfall &gt; 1.5 standard deviations of its long-term mean) over South Asia are associated with sea surface temperature (SST) anomalies over the equatorial Pacific during the developing phase of ENSO, and another 30% are associated with SST variations over the tropical Indo-Pacific warm pool. The present research aims to identify the moist processes that initiate the dryness

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42

Lee, David W. "Canopy dynamics and light climates in a tropical moist deciduous forest in India." Journal of Tropical Ecology 5, no. 1 (1989): 65–79. http://dx.doi.org/10.1017/s0266467400003229.

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ABSTRACTThe canopy dynamics and light climates within a 20 by 60 m quadrat were studied in a disturbed moist deciduous forest near Bombay, India. A map was drawn of individual trees within the quadrat, the taxa were identified, and their phenology was followed from November 1984 to July 1985. The quadrat contained 14 species, the most common being Tectona grandis, Terminalia tomentosa, Butea monosperma, Mitragyne parviflora and Albizia procera. Some individuals were in leaf at all times, more so at the moister east end of the quadrat. In November at the end of the rainy season, light measureme

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Rostami, M., and V. Zeitlin. "Understanding dynamics of large-scale atmospheric vortices with moist-convective shallow water model." Journal of Physics: Conference Series 738 (August 2016): 012055. http://dx.doi.org/10.1088/1742-6596/738/1/012055.

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Wang, Bin. "Dynamics of Tropical Low-Frequency Waves: An Analysis of the Moist Kelvin Wave." Journal of the Atmospheric Sciences 45, no. 14 (1988): 2051–65. http://dx.doi.org/10.1175/1520-0469(1988)045<2051:dotlfw>2.0.co;2.

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Spyksma, K., and P. Bartello. "Predictability in Wet and Dry Convective Turbulence." Journal of the Atmospheric Sciences 65, no. 1 (2008): 220–34. http://dx.doi.org/10.1175/2007jas2307.1.

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Abstract There is a growing interest in understanding the role that moisture plays in atmospheric dynamics, particularly in its effect on predictability. Current research indicates that when moisture effects are added to an atmospheric model, the error growth produced by the new moist dynamics reduces the predictability times, especially at the scales of moist convection. The issue of moist convection’s effect on predictability is addressed herein. By performing high-resolution large-ensemble runs, it is shown that although nonprecipitating moist convection is less predictable than dry convect

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Siegelman, Lia, Patrice Klein, Andrew P. Ingersoll, et al. "Moist convection drives an upscale energy transfer at Jovian high latitudes." Nature Physics 18, no. 3 (2022): 357–61. http://dx.doi.org/10.1038/s41567-021-01458-y.

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AbstractJupiter’s atmosphere is one of the most turbulent places in the solar system. Whereas observations of lightning and thunderstorms point to moist convection as a small-scale energy source for Jupiter’s large-scale vortices and zonal jets, this has never been demonstrated due to the coarse resolution of pre-Juno measurements. The Juno spacecraft discovered that Jovian high latitudes host a cluster of large cyclones with diameter of around 5,000 km, each associated with intermediate- (roughly between 500 and 1,600 km) and smaller-scale vortices and filaments of around 100 km. Here, we ana

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Yamada, Ray, and Olivier Pauluis. "Wave–Mean-Flow Interactions in Moist Baroclinic Life Cycles." Journal of the Atmospheric Sciences 74, no. 7 (2017): 2143–62. http://dx.doi.org/10.1175/jas-d-16-0329.1.

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Abstract Previous studies show that the moist Eliassen–Palm (EP) flux captures a greater eddy momentum exchange through form drag than the dry EP flux in the midlatitude climate. This suggests that the eddy moisture flux acts to decrease the baroclinicity of the zonal jet. This study investigates such a mechanism in moist baroclinic life cycles, which are simulated in an idealized general circulation model with large-scale condensation as the only moist process. The runs are analyzed using a linear diagnostic based on the Kuo–Eliassen equation to decompose the jet change into parts driven by i

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Dias, Juliana, and Olivier Pauluis. "Impacts of Convective Lifetime on Moist Geostrophic Adjustment." Journal of the Atmospheric Sciences 67, no. 9 (2010): 2960–71. http://dx.doi.org/10.1175/2010jas3405.1.

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Abstract This paper presents a theoretical study of the effects of moist convection on geostrophic adjustment in an infinite channel. The governing equations correspond to a linearized shallow water system of equations for the atmosphere first vertical baroclinic mode, which is coupled to a vertically averaged moisture equation. The coupling is through a parameterization that represents precipitation. The transient behavior and final state of the flow initially at rest with active precipitation limited to half of the channel is investigated, both numerically and analytically. It is shown that

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PÉLISSIER, RAPHAËL. "Tree spatial patterns in three contrasting plots of a southern Indian tropical moist evergreen forest." Journal of Tropical Ecology 14, no. 1 (1998): 1–16. http://dx.doi.org/10.1017/s0266467498000017.

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In a primary dense moist evergreen forest of southern India, spatial patterns of trees ≥30 cm gbh were investigated from three contrasting 0.4-ha plots that differed in topography and amount of disturbance due to treefall. Exploratory data analysis is based on second-order neighbourhood and pair-correlation statistics used to describe the degree of clustering/regularity in patterns of all trees, and the degree of attraction/repulsion between young trees and adults. Stochastic simulations from the Markov point process models are then used to fit spatial interaction models. The results show that

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Singh, H. P., and Samir Sarkar. "Vegetational dynamics of Tertiary Himalaya." Journal of Palaeosciences 38 (December 31, 1989): 333–44. http://dx.doi.org/10.54991/jop.1989.1668.

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Selected palaeobotanical and palynological records published from the Tertiary Period of Himalaya have been examined and a generalized vegetational frame work has been reconstructed. The diverse Palaeogene floras of Himalaya are marked by moist deciduous and wet semi-evergreen forest types growing mostly under tropical climate in varying type of environments. The tropical families register a decline in the Early Miocene time. The Middle Miocene Himalayan orogeny coincides with proliferation of Abietineae and by the appearance of several subtropical floral elements. Development and diversity of

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