Download or read book Effects of Precipitation on Ocean Mixed Layer Temperature and Salinity As Simulated in a 2 D Coupled Ocean Cloud Resolving Atmosphere Model written by Nasa Technical Reports Server (Ntrs) and published by BiblioGov. This book was released on 2013-06 with total page 42 pages. Available in PDF, EPUB and Kindle. Book excerpt: The NASA Technical Reports Server (NTRS) houses half a million publications that are a valuable means of information to researchers, teachers, students, and the general public. These documents are all aerospace related with much scientific and technical information created or funded by NASA. Some types of documents include conference papers, research reports, meeting papers, journal articles and more. This is one of those documents.

Download or read book Cloud Resolving Modeling of Convective Processes written by Xiaofan Li and published by Springer. This book was released on 2016-05-17 with total page 364 pages. Available in PDF, EPUB and Kindle. Book excerpt: This is an updated and revised second edition of the book presenting new developments in the field of cloud-resolving modeling. The first edition of the book introduces the framework of cloud-resolving model, methodologies for analysis of modeling outputs, and validation of simulations with observations. It details important scientific findings in the aspects of surface rainfall processes, precipitation efficiency, dynamic and thermodynamic processes associated with tropical convection, diurnal variations, radiative and cloud microphysical processes associated with development of cloud clusters, air-sea coupling on convective scales, climate equilibrium states, and remote sensing applications. In additional to the content from the first edition of the book, the second edition of the book contains the new scientific results in the development of convective-stratiform rainfall separation scheme, the analysis of structures of precipitation systems, the thermal effects of doubled carbon dioxide on rainfall, precipitation predictability, and modeling depositional growth of ice crystal. The book will be beneficial both to graduate students and to researchers who do cloud, mesoscale and global modeling.

Download or read book Observation Theory and Modeling of Atmospheric Variability written by Xun Zhu and published by World Scientific. This book was released on 2004 with total page 644 pages. Available in PDF, EPUB and Kindle. Book excerpt: This book contains tutorial and review articles as well as specific research letters that cover a wide range of topics: (1) dynamics of atmospheric variability from both basic theory and data analysis, (2) physical and mathematical problems in climate modeling and numerical weather prediction, (3) theories of atmospheric radiative transfer and their applications in satellite remote sensing, and (4) mathematical and statistical methods. The book can be used by undergraduates or graduate students majoring in atmospheric sciences, as an introduction to various research areas; and by researchers and educators, as a general review or quick reference in their fields of interest.

Download or read book Cloud Resolving Modeling of Convective Processes written by Shouting Gao and published by Springer Science & Business Media. This book was released on 2008-04-03 with total page 213 pages. Available in PDF, EPUB and Kindle. Book excerpt: Clouds and cloud systems and their interactions with larger scales of motion, radiation, and the Earth’s surface are extremely important parts of weather and climate systems. Their treatment in weather forecast and climate models is a significant source of errors and uncertainty. As computer power increases, it is beginning to be possible to explicitly resolve cloud and precipitation processes in these models, presenting opportunities for improving precipitation forecasts and larger-scale phenomena such as tropical cyclones which depend critically on cloud and precipitation physics. This book by Professor Shouting Gao of the Institute of Atmospheric Physics in Beijing and Xiaofan Li of NOAA’s National Environmental Satellite Data and Information Services (NESDIS) presents an update and review of results of high-resolution, mostly two-dimensional models of clouds and precipitation and their interactions with larger scales of motion and the Earth’s surface. It provides a thorough description of cloud and precipitation physics, including basic governing equations and related physics, such as phase changes of water, radiation and mixing. Model results are compared with observations from the 1992-93 Tropical Ocean Global Atmosphere Coupled Ocean Atmosphere Response Experiment (TOGA COARE) experiment. The importance of the ocean to tropical convective systems is clearly shown here in the numerical results of simulations with their air-sea coupled modeling system. While the focus is on tropical convection, the methodology and applicability can be extended to cloud and precipitation processes elsewhere. The results described in this well-written book form a solid foundation for future high-resolution model weather forecasts and climate simulations that resolve clouds explicitly in three dimensions—a future that has great promise for the understanding and prediction of weather and climate for the great benefit of society.

Download or read book Effect of Cloud Precipitation Ocean Mixed Layer Feedback on Drag Coefficient written by and published by . This book was released on 1992 with total page 5 pages. Available in PDF, EPUB and Kindle. Book excerpt: From similarity theory, the drag and thermal exchange coefficients (C(D), C(H), and C(E)) for 10m above the ocean surface depend on the atmospheric stability parameter (z/L(alpha)) where L(alpha) the Obukhov length scale for the atmospheric surface layer. Cloud, precipitation, and ocean mixed layer (OML) thermodynamical feedback affects the atmospheric stability parameter in two ways. Clouds reduce the incoming solar radiation at the ocean surface by scattering and absorption, which cools (relatively) the ocean mixed layer. The OML cooling lowers the sensible and latent heat fluxes from the ocean surface, which increases the atmospheric stability parameter. On the other hand, precipitation from the clouds dilutes the surface salinity, stabilizing the upper ocean, and reducing OML deepening. The ocean mixed layer may be caused to shallow if the downward surface buoyance flux is sufficiently enhanced by the precipitation. When the ocean surface receives a downward net surface heat flux, the reduction in the OML depth will increase the sea surface temperature (SST) by concentrating the net radiation plus heat fluxed downward across the sea surface into a thinner layer. The increase of SST augments the sensible and latent heat fluxes from the ocean surface, which decreases the atmospheric stability parameter. On the other hand, when the ocean surface has a net surface heat loss, the reduction in the OML depth will decrease SST due to the decrease of the thermal inertia. The decrease of SST reduces the sensible and latent heat fluxes from the ocean surface, which increases the atmospheric stability parameter. The variation of atmospheric stability parameter in turn changes the drag and thermal exchange coefficients. In this study, a simple coupled cloud-precipitation- ocean mixed layer model proposed by Chu et. al. (1990) and Chu and Garwood (1991) is used to compute the time rate change of drag and thermal exchange coefficients caused by this mechanism.

Download or read book Recent Progress in Atmospheric Sciences written by K. N. Liou and published by World Scientific. This book was released on 2008 with total page 497 pages. Available in PDF, EPUB and Kindle. Book excerpt: This book contains 22 peer-reviewed articles that cover a spectrum of contemporary subjects relevant to atmospheric sciences, with specific applications to the Asia-Pacific region. The majority of these papers consist of a review of a scientific sub-field in atmospheric sciences, while some contain original contributions. All of the accepted papers were subject to scientific reviews and revisions.

Download or read book Next Generation Earth System Prediction written by National Academies of Sciences, Engineering, and Medicine and published by National Academies Press. This book was released on 2016-08-22 with total page 351 pages. Available in PDF, EPUB and Kindle. Book excerpt: As the nation's economic activities, security concerns, and stewardship of natural resources become increasingly complex and globally interrelated, they become ever more sensitive to adverse impacts from weather, climate, and other natural phenomena. For several decades, forecasts with lead times of a few days for weather and other environmental phenomena have yielded valuable information to improve decision-making across all sectors of society. Developing the capability to forecast environmental conditions and disruptive events several weeks and months in advance could dramatically increase the value and benefit of environmental predictions, saving lives, protecting property, increasing economic vitality, protecting the environment, and informing policy choices. Over the past decade, the ability to forecast weather and climate conditions on subseasonal to seasonal (S2S) timescales, i.e., two to fifty-two weeks in advance, has improved substantially. Although significant progress has been made, much work remains to make S2S predictions skillful enough, as well as optimally tailored and communicated, to enable widespread use. Next Generation Earth System Predictions presents a ten-year U.S. research agenda that increases the nation's S2S research and modeling capability, advances S2S forecasting, and aids in decision making at medium and extended lead times.

Download or read book Impact of the Current Feedback and Model Resolution on the Atmosphere and Ocean Mixed Layer Over the Gulf Stream written by Jackie Crystal May and published by . This book was released on 2022 with total page 0 pages. Available in PDF, EPUB and Kindle. Book excerpt: The atmosphere and the ocean interact through air-sea heat and momentum fluxes. Thesefluxes are critical in ocean, atmosphere, and coupled modeling across a broad range of spatial and temporal scales, from large-scale global modeling to very high-resolution regional studies and from climate studies to operational forecasting. It is important to minimize the air-sea flux errors in order to obtain accurate and realistic model results. This study investigates two sources of air-sea flux errors within the Gulf Stream region during winter months: the horizontal model resolution of the atmosphere and the ocean, and the dynamical coupling and current feedback between the ocean surface currents and the wind stress. Four different atmospheric and ocean coupled model simulations are completed with various combinations of 2 km (submesoscale resolving) and 6 km (submesoscale permitting) grid spacing. Four additional model simulations are completed using the same model resolutions defined in the first four experiments, but the coupling and feedback between the surface currents and the wind stress is included. The dynamical coupling and the current feedback lead to large changes in the surfacestress and stress curl patterns. This leads to a reduction in the ocean's mean and eddy kinetic energy, which largely controls the Gulf Stream path. The dynamical coupling is also found to control the physical gradient related to the atmospheric horizontal momentum advection. The stress gradient largely explains the variability in the horizontal advection when the dynamical coupling is not included, while the current gradient across current direction largely explains the variability in the horizontal advection when the dynamical coupling is included. Additionally, the dynamical coupling and current feedback is found to be important in regulating the mixed layer depth and SST throughout the warm water to the right of the Gulf Stream path due to the horizontal heat advection in the mixed layer. A high-resolution ocean model is found to also be important in influencing the Gulf Stream path, as well as constraining the submesoscale vertical heat fluxes to the ocean's mixed layer. The atmospheric model resolution is found to impact the magnitude of the stress, wind work, sea surface height, and surface currents, in addition to the strength of the horizontal and vertical winds throughout the atmospheric column. The dynamical coupling and current feedback, as well as having a high-resolution atmosphere and ocean, is further found to be important in the vertical extent of the state parameter fields, as well as in the atmospheric circulation patterns.

Download or read book Discrete Precipitation Effects on Seasonal Mixed Layer Dynamics in the North Pacific Ocean written by Mendal S. Livezey and published by . This book was released on 1988 with total page 80 pages. Available in PDF, EPUB and Kindle. Book excerpt: This study was conducted to examine the effects of discrete precipitation events on the short-term and seasonal evolution of ocean mixed layer temperature and salinity structure. Two numerical modeling experiments were performed. The first was to simulate the response of the mixed layer to hypothetical discrete (isolated) precipitation events. This experiment showed that the effect of a single discrete rain event can vary with season, with the mixed layer depth (MLD) at onset of the rain event, and with the strength of wind stress forcing. A single rain event can have lasting effects on mixed layer depth and temperature for up to 55 days after the event, depending upon the season. The second experiment simulated quasi-realistic complex precipitation forcing, with a realistic distribution of synoptic events over a 13-month period. For this experiment, four different precipitation intensities were tested. The values of temperature, salinity, and MLD predicted by the model were compared with observed Conductivity Temperature Depth measurements and with the values predicted using constant precipitation forcing. Keywords: Military theses, Oceanography, Air-sea interaction, Mixed layer modeling. (kt).

Download or read book Intraseasonal Variability in the Atmosphere Ocean Climate System written by William K.-M. Lau and published by Springer Science & Business Media. This book was released on 2007-06-10 with total page 477 pages. Available in PDF, EPUB and Kindle. Book excerpt: This is the first comprehensive review of intra-seasonal variability (ISV); the contents are balanced between observation, theory and modeling. Starting with an overview of ISV and historical observations, the book addresses the coupling between ocean and atmosphere, and the worldwide role of ISV in monsoon variability. Also considered are the connections between oscillations like the Madden, Julian and El Nino/Southern and short-term climate.

Download or read book Dissertation Abstracts International written by and published by . This book was released on 2005 with total page 918 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Download or read book Coupled Ocean atmosphere Models written by Jacques C. J. Nihoul and published by Elsevier Publishing Company. This book was released on 1985 with total page 800 pages. Available in PDF, EPUB and Kindle. Book excerpt: The exchange of momentum, heat, moisture, gases (such as CO 2 and O 2 ) and salt between the atmosphere and the ocean is a phenomenon of paramount importance for the dynamics of the atmosphere and the ocean. With the pressing need for reliable climate forecast (e.g. to deal with severe food and energy problems) interactive ocean-atmosphere models have become one of the main objectives of geophysical fluid dynamics. This volume provides the first state-of-the-art review of interactive ocean-atmosphere modelling and its application to climates. The papers are by active and eminent scientists from different countries and different disciplines. They provide a up-to-date survey of major recent discoveries and valuable recommendations for future research."

Download or read book Thermodynamic Feedback Between Clouds and the Ocean Surface Mixed Layer written by and published by . This book was released on 1989 with total page 11 pages. Available in PDF, EPUB and Kindle. Book excerpt: A cloud-ocean planetary boundary layer (OPBL) feedback mechanism is presented and tested in this paper. Water vapor, evaporated from the ocean surface or transported by the large-scale air flow, often forms convective clouds under a conditionally unstable lapse rate. The variable cloud cover and rainfall may base positive and negative feedback with the ocean mixed layer temperature and salinity structure. The coupling of the simplified Kuo's (1965) cumulus cloud model to the Kraus-Turner's (1967) ocean mixed layer model shows the existence of this feedback mechanism. The theory also predicts the generation of low frequency oscillation in the atmosphere and oceans.

Download or read book The Impact of Air sea Interactions on the Simulation of Tropical Intraseasonal Variability written by Kathy Pegion and published by . This book was released on 2007 with total page 62 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Download or read book Natural Climate Variability on Decade to Century Time Scales written by National Research Council and published by National Academies Press. This book was released on 1996-08-30 with total page 645 pages. Available in PDF, EPUB and Kindle. Book excerpt: This volume reflects the current state of scientific knowledge about natural climate variability on decade-to-century time scales. It covers a wide range of relevant subjects, including the characteristics of the atmosphere and ocean environments as well as the methods used to describe and analyze them, such as proxy data and numerical models. They clearly demonstrate the range, persistence, and magnitude of climate variability as represented by many different indicators. Not only do natural climate variations have important socioeconomic effects, but they must be better understood before possible anthropogenic effects (from greenhouse gas emissions, for instance) can be evaluated. A topical essay introduces each of the disciplines represented, providing the nonscientist with a perspective on the field and linking the papers to the larger issues in climate research. In its conclusions section, the book evaluates progress in the different areas and makes recommendations for the direction and conduct of future climate research. This book, while consisting of technical papers, is also accessible to the interested layperson.

Download or read book Global Physical Climatology written by Dennis L. Hartmann and published by Academic Press. This book was released on 1994-07-06 with total page 425 pages. Available in PDF, EPUB and Kindle. Book excerpt: Global Physical Climatology is an introductory text devoted to the fundamental physical principles and problems of climate sensitivity and change. Addressing some of the most critical issues in climatology, this text features incisive coverage of topics that are central to understanding orbital parameter theory for past climate changes, and for anthropogenic and natural causes of near-future changes--Key Features* Covers the physics of climate change* Examines the nature of the current climate and its previous changes* Explores the sensitivity of climate and the mechanisms by which humans are likely to produce near-future climate changes* Provides instructive end-of-chapter exercises and appendices

Download or read book Salinity Effects in an Ocean Mixed Layer Model written by Richard Alan Paulus and published by . This book was released on 1978 with total page 76 pages. Available in PDF, EPUB and Kindle. Book excerpt: A one-dimensional mixed-layer model of ocean thermal structure (Camp, 1976) was first modified to determine the effects of a salinity profile on density structure and secondly to observe the added effects of surface salinity flux. The model was tested in August and November-December 1974 with (1) hydrocast data at Ocean Stations HOTEL and PAPA and (2) salinity profiles statistically derived from historical data for six ocean stations and adjusted to correspond to an observed BT. Inclusion of salinity structure did not significantly affect mixed-layer depth or temperature predictions during the summer period. During the winter period, salinity structure tended to inhibit deepening yielding a slightly warmer, shallower mixed layer. Surface salinity flux altered significantly the thickness of the isothermal layer, with decreases in thickness during precipitation (E-P0) and a tendency for increased thickness during some periods of net downward heat flux when E-P0. (Author).