標(biāo)題: Titlebook: Current Trends in the Representation of Physical Processes in Weather and Climate Models; David A. Randall,J. Srinivasan, Parthasarathi Mu [打印本頁] 作者: 可入到 時(shí)間: 2025-3-21 18:45
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書目名稱Current Trends in the Representation of Physical Processes in Weather and Climate Models讀者反饋學(xué)科排名
作者: Pathogen 時(shí)間: 2025-3-21 23:16
Challenges in Tropical Numerical Weather Prediction at ECMWF,is our benchmark. These challenges comprise four main areas of developments: making optimal use of the available observational data to obtain the best analysis, advanced ensemble methods to predict the uncertainties in the analyses and forecasts, model developments to better represent shallow and de作者: FILTH 時(shí)間: 2025-3-22 02:47
Convection Initiation in Climate Models Using the Heated Condensation Framework: A Review,f parameterizing convection based on parcel theory. Formulated to take into account the role of atmospheric mixing within the boundary layer, the HCF uses profiles of temperature and humidity to quantify how conditioned the atmosphere is to moist free convection. The initiation of convection is eval作者: famine 時(shí)間: 2025-3-22 06:10
Cloud Microphysics Across Scales for Weather and Climate,thods used for representing microphysical processes in weather and climate models, from explicit bin schemes used for small-scale simulation up to bulk treatments often used in global models. Of particular importance is how the cloud microphysical treatments are coupled to the rest of the cloud sche作者: ANIM 時(shí)間: 2025-3-22 10:18 作者: Basilar-Artery 時(shí)間: 2025-3-22 13:25 作者: Basilar-Artery 時(shí)間: 2025-3-22 17:31 作者: 吹牛需要藝術(shù) 時(shí)間: 2025-3-23 00:56 作者: 可卡 時(shí)間: 2025-3-23 04:36 作者: Crater 時(shí)間: 2025-3-23 07:58 作者: 美麗的寫 時(shí)間: 2025-3-23 09:46
Difficulties in the Subgrid-Scale Redistribution of Moisture of a Global Cloud-Resolving Model,resolution global simulations have been beneficial not only to advance our knowledge of organized cloud systems but also to give various hints on improvements of traditional global models that depend on a kind of cumulus parameterization, explicit computations of cloud microphysics cannot necessaril作者: 步履蹣跚 時(shí)間: 2025-3-23 17:24 作者: Processes 時(shí)間: 2025-3-23 21:16 作者: 骨 時(shí)間: 2025-3-24 02:16
Microphysics in Goddard Multi-scale Modeling Systems: A Review,ncreasingly more sophisticated physical parameterizations. The representation of cloud microphysical processes is one of the key components of these models. In addition, over the past decade, both research and operational numerical weather prediction models have started using more complex microphysi作者: 憤慨點(diǎn)吧 時(shí)間: 2025-3-24 04:11 作者: Osteons 時(shí)間: 2025-3-24 07:52
New Pathways for Moist Convection Parameterisation,models. The shortcomings of this approach will be discussed, especially for higher resolutions where standard assumptions such as quasi-equilibrium start to break down. New pathways that use a stochastic approach and are scale aware will be discussed. These will also allow to incorporate the effect 作者: Orthodontics 時(shí)間: 2025-3-24 11:22
Land Surface Processes,k for the land surface and land–atmosphere coupling processes. This is followed by a discussion regarding the role and the need for improving land feedbacks within multiscale models and processes. In particular, the role of land surface models in providing surface boundary conditions within numerica作者: spinal-stenosis 時(shí)間: 2025-3-24 18:04
Current Trends in the Representation of Physical Processes in Weather and Climate Models978-981-13-3396-5Series ISSN 2194-5217 Series E-ISSN 2194-5225 作者: 沒花的是打擾 時(shí)間: 2025-3-24 19:23
https://doi.org/10.1007/978-3-662-61766-3nd joint probability distribution—have not received much scrutiny, let alone validation against actual observations. This leads to some very problematic inconsistencies, which are described in this chapter, along with guidance on approaches to resolve them objectively.作者: Abjure 時(shí)間: 2025-3-25 00:13 作者: 不可接觸 時(shí)間: 2025-3-25 05:28
https://doi.org/10.1007/978-3-662-61740-3ipitation annual cycle accurately. Here, we review and examine the nature and dynamical causes of their biases. We discuss the coupled nature of the monsoon annual cycle from observations and then present errors in multi-model-mean, climatological fields of ocean–atmosphere variables determined from作者: 完全 時(shí)間: 2025-3-25 08:24
https://doi.org/10.1007/978-3-662-61766-3is our benchmark. These challenges comprise four main areas of developments: making optimal use of the available observational data to obtain the best analysis, advanced ensemble methods to predict the uncertainties in the analyses and forecasts, model developments to better represent shallow and de作者: 厭煩 時(shí)間: 2025-3-25 14:56
Petrus Apianus und der Dreisatzf parameterizing convection based on parcel theory. Formulated to take into account the role of atmospheric mixing within the boundary layer, the HCF uses profiles of temperature and humidity to quantify how conditioned the atmosphere is to moist free convection. The initiation of convection is eval作者: lymphoma 時(shí)間: 2025-3-25 18:51 作者: Lignans 時(shí)間: 2025-3-25 22:53 作者: 肥料 時(shí)間: 2025-3-26 01:34
Wie kommt man auf Quaternionen?n of Indian summer monsoon. The location of maximum precipitation and CAPE does not always coincide in a CRM simulation. The diurnal land surface heating is shown to have an effect on CAPE and precipitation over ocean. Convective inhibition energy is shown to have a significant effect on the locatio作者: Acumen 時(shí)間: 2025-3-26 08:16 作者: 捕鯨魚叉 時(shí)間: 2025-3-26 11:17
https://doi.org/10.1007/978-3-662-62562-0ast System version 2 (CFSV2). The resulting model is referred to here as CFSsmcm. Two 15-year-long climate simulations of the CFSsmcm, differing only by one SMCM parameter, namely, the mid-tropospheric dryness parameter, MTD0 are analyzed and interpreted here. This particular parameter is chosen bec作者: zonules 時(shí)間: 2025-3-26 14:59
Regina Toepfer,Peter Burschel,J?rg Weschenstitute of Tropical Meteorology, in order to address key questions pertaining to the science of Climate Change. The IITM-ESM has been developed by transforming a state-of-the-art seasonal prediction model into a radiatively balanced climate modeling framework suitable for investigating long-term cl作者: 連鎖 時(shí)間: 2025-3-26 18:46 作者: Influx 時(shí)間: 2025-3-26 22:48
https://doi.org/10.1007/978-3-662-62562-0resolution global simulations have been beneficial not only to advance our knowledge of organized cloud systems but also to give various hints on improvements of traditional global models that depend on a kind of cumulus parameterization, explicit computations of cloud microphysics cannot necessaril作者: Epithelium 時(shí)間: 2025-3-27 01:34 作者: MORT 時(shí)間: 2025-3-27 05:29
Einführung zum transzendentalen Idealismuswhich can be applied for decision-making in different sectors like agriculture, power distribution, disaster management and water resource management. Forecasting of monsoon weather system and associated rainfall is one of the most difficult areas in NWP due to complexities in land–ocean–atmosphere 作者: 中世紀(jì) 時(shí)間: 2025-3-27 12:12 作者: irreducible 時(shí)間: 2025-3-27 15:02
?Das musikalische Drama der Zukunft?uidance for public since December 1992. Since July 2017, the GEFS was extended from 16?days to 35?days forecast to support NCEP Climate Prediction Center (CPC)’s sub-seasonal forecast. The latest GEFS version was upgraded in three areas to improve sub-seasonal forecast: (1) introducing a new set of 作者: 免費(fèi) 時(shí)間: 2025-3-27 17:57 作者: DEAWL 時(shí)間: 2025-3-27 23:40 作者: Collar 時(shí)間: 2025-3-28 04:42 作者: 責(zé)問 時(shí)間: 2025-3-28 07:58
Springer Nature Singapore Pte Ltd. 2019作者: 贊美者 時(shí)間: 2025-3-28 12:38 作者: 慷慨不好 時(shí)間: 2025-3-28 15:19 作者: PANIC 時(shí)間: 2025-3-28 18:59 作者: gorgeous 時(shí)間: 2025-3-29 00:47
Convection Initiation in Climate Models Using the Heated Condensation Framework: A Review,ate perspective, applying the HCF trigger to the Community Earth System Model reduces convective overactivity in the model and improves the frequency of intense precipitation events. The use of the HCF as a convective trigger is still under active investigation, and strategies for including the effe作者: Inoperable 時(shí)間: 2025-3-29 04:30
Convective Available Potential Energy and Precipitation in a Cloud-Resolving Model Simulation of Innot include any representation of organized mesoscale convective systems. We show that CAPE consumed by these systems not only triggers vertical motion but also contributes to horizontal motion of the system.作者: 兩棲動(dòng)物 時(shí)間: 2025-3-29 08:03
A Gray Zone GCM with Full Representation of Cloud Microphysics,equencies and the MJO reasonably well, although the MJO intensity is rather strong. Both cloud microphysics and scale-dependent deep convection play important roles in simulating a realistic MJO in the present GCM. Also noted is that the precipitation climatologies of the present atmospheric GCM (AG作者: 知識分子 時(shí)間: 2025-3-29 15:25 作者: 膠水 時(shí)間: 2025-3-29 16:00
Cumulus Friction in the Asian Monsoon of a Global Model with 7 km Mesh,ection and shear are both strong, the viscosity can be characterized by a regression coefficient with values of about 5% cm., meaning that convection which yields 1 cm of precipitation decrements SKE by about 5%. Adjustment of balanced monsoon flow to such a viscous effect implies adiabatic ascent t作者: 不連貫 時(shí)間: 2025-3-29 20:13 作者: 不透明 時(shí)間: 2025-3-30 02:55 作者: 自然環(huán)境 時(shí)間: 2025-3-30 04:27 作者: nascent 時(shí)間: 2025-3-30 11:58 作者: 同音 時(shí)間: 2025-3-30 13:00 作者: 植物群 時(shí)間: 2025-3-30 19:20
Current Trends in the Representation of Physical Processes in Weather and Climate Models作者: 癡呆 時(shí)間: 2025-3-31 00:42
2194-5217 ection and grid-scale cloud microphysics and its impact on models’ intrinsic predictability, the book offers a motivating reference guide for all researchers whose work involves physical parameterization problems and numerical models.978-981-13-3396-5Series ISSN 2194-5217 Series E-ISSN 2194-5225 作者: 熄滅 時(shí)間: 2025-3-31 03:30
Book 2019ging debate on the cloud-resolving approach or the hybrid approach with parameterized convection and grid-scale cloud microphysics and its impact on models’ intrinsic predictability, the book offers a motivating reference guide for all researchers whose work involves physical parameterization problems and numerical models.作者: 膽大 時(shí)間: 2025-3-31 06:33
https://doi.org/10.1007/978-3-662-61740-3ls suggests that multiple processes and their interactions lead to these persistent errors. We review recent literature that addressed the source(s) of model errors and indicate the importance of examining both atmospheric and oceanic fast processes. After discussing the unique nature of observed co作者: DIKE 時(shí)間: 2025-3-31 11:27
Petrus Apianus und der Dreisatzate perspective, applying the HCF trigger to the Community Earth System Model reduces convective overactivity in the model and improves the frequency of intense precipitation events. The use of the HCF as a convective trigger is still under active investigation, and strategies for including the effe作者: 懦夫 時(shí)間: 2025-3-31 16:59
Wie kommt man auf Quaternionen?not include any representation of organized mesoscale convective systems. We show that CAPE consumed by these systems not only triggers vertical motion but also contributes to horizontal motion of the system.作者: 平靜生活 時(shí)間: 2025-3-31 18:39
,Ziel erreicht: die ersten Tage?…,equencies and the MJO reasonably well, although the MJO intensity is rather strong. Both cloud microphysics and scale-dependent deep convection play important roles in simulating a realistic MJO in the present GCM. Also noted is that the precipitation climatologies of the present atmospheric GCM (AG
