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  • 1
    Keywords: Lilly, D. K. ; Atmospheric turbulence ; Mesometeorology ; Numerical weather forecasting ; Bibliografie ; Aufsatzsammlung ; Atmosphärische Turbulenz ; Mesometeorologie ; Numerische Wettervorhersage
    Type of Medium: Online Resource
    Pages: ill (some col.), ports
    Edition: Online-Ausg. Online-Ressource (PDF-Datei: X, 280 S., MB/KB)
    ISBN: 9780511735035
    DDC: 551.55
    RVK:
    Language: English
    Note: Includes bibliographical references and index , Formerly CIP , Systemvoraussetzungen:
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  • 2
    Online Resource
    Online Resource
    Cham :Springer International Publishing AG,
    Keywords: Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (396 pages)
    Edition: 1st ed.
    ISBN: 9783319772738
    Series Statement: Space Sciences Series of ISSI Series ; v.65
    Language: English
    Note: Intro -- Contents -- Preface to the Special Issue ''ISSI Workshop on Shallow Clouds and Water Vapor, Circulation and Climate Sensitivity'' -- 1 Convective Self-Aggregation in Numerical Simulations: A Review -- 1 Introduction -- 2 Characteristics of Self-Aggregation -- 2.1 General Evolution of Aggregation -- 2.2 Identifying Metrics -- 2.3 Time Scale -- 2.4 Length Scale -- 2.5 Impacts -- 3 Mechanisms of Self-Aggregation -- 3.1 Surface Fluxes -- 3.1.1 Sensitivity to SST -- 3.2 Longwave Radiation -- 3.2.1 Sensitivity to SST -- 3.3 Shortwave Radiation -- 3.3.1 Sensitivity to SST -- 3.4 Advective Processes -- 3.5 Moisture Feedbacks -- 3.6 Triggering Versus Maintenance -- 4 Importance of Self-Aggregation -- 5 Conclusions -- 5.1 What Aspects of Self-Aggregation do Modeling Studies Agree on? -- 5.2 What Remains Uncertain? -- 5.3 What Could be Explored More? -- 5.4 Synthesis -- References -- 2 Observing Convective Aggregation -- 1 Introduction -- 1.1 Importance of Aggregation -- 1.2 Literature Review: Observational Studies of Convective Organization -- 2 Observational Perspectives on Processes Important for Idealized Convective Aggregation -- 2.1 Metrics to Quantify Feedbacks -- 2.2 Initiation Processes -- 2.2.1 Longwave Radiation -- 2.2.2 Surface Fluxes -- 2.2.3 Shortwave Radiation -- 2.2.4 Moisture-Convection Feedbacks -- 2.3 Sensitivity to SST -- 2.4 Maintenance Processes -- 3 Comparing the Idealized World to the Natural World -- 3.1 Time Scales of Self-Aggregation -- 3.2 Mean Wind and Wind Shear -- 3.3 Humidity Profiles -- 3.4 Equatorial Wave Dynamics -- 3.5 Ocean Interaction and Feedback -- 4 Observational Perspectives on Aggregation in a Warming Climate -- 5 Future Observational Aspirations -- 5.1 Evolution of Convective Organization Using Satellite Data -- 5.2 Spaceborne Cloud Radar Approaches. , 5.3 Feasibility of a Ground-Based Observational Network -- 6 Conclusions -- References -- 3 An Observational View of Relationships Between Moisture Aggregation, Cloud, and Radiative Heating Profiles -- 1 Introduction -- 2 Characterizing Aggregation in Clouds and Their Environment -- 2.1 Observations from the A-Train -- 2.2 Characterizing Aggregation in the Water Vapor Field -- 3 Relationships Among Clouds, Humidity, and Aggregation -- 3.1 Cloudiness Depends on Sea Surface Temperature and Aggregation State -- 3.2 Cloudiness, Radiative Heating, and Convective Intensity -- 3.3 Does Vapor Aggregation Imply Convective Aggregation? -- 4 Summary and Discussion -- References -- 4 Correction to: An Observational View of Relationships Between Moisture Aggregation, Cloud, and Radiative Heating Profiles -- 5 Implications of Warm Rain in Shallow Cumulus and Congestus Clouds for Large-Scale Circulations -- 1 Introduction -- 2 Warm Rain in Large-Scale Circulations -- 2.1 A Two-Column RCE Model -- 2.2 Circulating Equilibria in the Two-Column System -- 2.3 Shallow Cumulus -- 2.4 Congestus -- 3 From a Conceptual Model to Nature -- 3.1 Large-Eddy Simulations -- 3.2 Observations -- 4 Concluding Thoughts -- References -- 6 A Survey of Precipitation-Induced Atmospheric Cold Pools over Oceans and Their Interactions with the Larger-Scale Environment -- 1 Introduction -- 2 Cold Pools from Boundary Layers not Exceeding 2 km Altitude -- 3 Cold Pools from Convection Reaching the Mid-Troposphere -- 4 Cold Pools from Deep Tropical Convection -- 5 Remaining Questions -- 5.1 The Relationship of Trade Wind Cold Pools to Cloud Cover -- 5.2 Thermodynamic Secondary Initiation Processes -- References -- 7 Low-Cloud Feedbacks from Cloud-Controlling Factors: A Review -- 1 Seeking Observational Constraints on Low-Cloud Feedbacks -- 2 Cloud-Controlling Factors -- 3 Low-Cloud Feedbacks. , 4 Implications for Climate Sensitivity -- 5 Sources of Uncertainty -- 5.1 Fundamental Issues -- 5.1.1 F1. Are Cloud Sensitivities Time-scale Invariant? -- 5.1.2 F2. Are Clouds Responding to the Controlling Factors? -- 5.1.3 F3. Uncertainty in the Climate Change Prediction of Cloud-Controlling -- Factors -- 5.1.4 F4. Time-Dependency of Cloud-Controlling Factors During a Climate Change -- 5.2 Implementation Issues -- 5.2.1 I1. Imperfect Observations of Clouds and Their Controlling Factors -- 5.2.2 I2. Limited Duration of the Observational Record -- 5.2.3 I3. Limited Spatial Sampling of the Observations -- 5.2.4 I4. Imprecise Statistical Modeling -- 5.2.5 I5. Incomplete Set of Cloud-Controlling Factors -- 6 Summary and Final Remarks -- References -- 8 Mechanisms and Model Diversity of Trade-Wind Shallow Cumulus Cloud Feedbacks: A Review -- 1 Introduction -- 2 Interpreting Model Differences in Trade-Wind Cloud Responses to Warming in General Circulation Models -- 2.1 Boundary-Layer Moisture Budget -- 2.2 The Role of Shallow Convective Mixing -- 3 A Mass Budget Perspective on Cloud-Base Cloud Fraction -- 4 High-Resolution Simulation of Shallow Cumulus Cloud Changes and Mechanisms -- 4.1 Trade-Wind Shallow Cumulus Cloud Response to Warming in LES -- 4.1.1 The Role of Precipitation -- 4.1.2 The Role of Organization -- 4.2 Robustness and Uncertainties of LES Studies -- 5 Connecting LES and GCM Interpretations of Shallow Cumulus Cloud Feedback Mechanisms -- 6 Observational Support for Trade-Wind Shallow Cumulus Cloud Feedbacks -- 7 Synthesis -- References -- 9 Importance Profiles for Water Vapor -- 1 Introduction -- 2 Simplest: The Profile of -- Mass Errors from Vapor Measurement Errors -- 3 Radiative Kernels: Sensitivity of OLR to Humidity -- 4 Importance of Vapor for Deep Convection -- 5 Importance Functions for Passive Remote Sensing. , 6 Summary and Conclusions -- References -- 10 Structure and Dynamical Influence of Water Vapor in the Lower Tropical Troposphere -- 1 Introduction -- 2 Data and Context -- 2.1 Airborne Measurements and the Barbados Cloud Observatory -- 2.1.1 Dropsonde Humidity Measurements During the NARVAL Campaigns -- 2.1.2 WALES -- 2.2 SAPHIR and Megha-Tropiques -- 2.3 Infrared Atmospheric Sounding Interferometer (IASI) -- 3 How Lower-Tropospheric Humidity Influences Clouds, Convection and Circulation -- 3.1 Humidity in the Planetary Boundary Layer -- 3.2 Column Water Vapor (Thermodynamic Effects) -- 3.3 Column Water Vapor (radiative effects) -- 3.4 Elevated Moist Layers -- 4 Remotely Sensed Humidity Variations During NARVAL-1 and NARVAL-2 -- 4.1 General Structure of Humidity Retrievals from SAPHIR -- 4.2 Evaluation of SAPHIR Retrievals by WALES -- 4.3 Comparison with IASI and the Added Value of Retrieving Isotopologues -- 5 A Hypothesis for the Preponderance of Melting Level Convection -- 6 Conclusions -- References -- 11 The Representation of Tropospheric Water Vapor Over Low-Latitude Oceans in (Re-)analysis: Errors, Impacts, and the Ability to Exploit Current and Prospective Observations -- 1 Tropospheric Water Vapor Over Low-Latitude Oceans -- 2 Integrating Observations in Space and Time: Data Assimilation and (Re-)analysis -- 2.1 Producing Meteorological (Re-)analyses -- 2.1.1 Global Forecast Models -- 2.1.2 Data Assimilation Systems -- 2.1.3 Challenges in Assimilating Moisture -- 2.2 Analysis and Reanalysis -- 3 What Measurements Inform Current Estimates? -- 3.1 Microwave and Infrared Sounding -- 3.1.1 Principles of Measurement -- 3.1.2 Why Both Microwave and Infrared Observations are Useful -- 3.1.3 Prospects -- 3.2 Estimates of Precipitable Water from Microwave Observations -- 3.3 GNSS Radio Occultation: A Global Refractometer. , 3.3.1 Principles of Measurement -- 3.3.2 Vertical Resolution, Accuracy, and Limitations -- 3.3.3 Prospects -- 4 Errors in Water Vapor Distributions and the Resulting Impacts -- 4.1 Assessing Errors in the Analyzed Distribution of Water Vapor -- 4.1.1 Assessment in Subsiding Regions -- 4.1.2 Assessment in Convecting Regions -- 4.2 Assessing Impacts -- 5 Characterizing Water Vapor in a More Richly Observed World -- 5.1 Limited Observations and Model Error -- 5.2 Exploiting Richer Observations -- References -- 12 Airborne Lidar Observations of Water Vapor Variability in Tropical Shallow Convective Environment -- 1 Introduction -- 2 The DLR Airborne Water Vapor Lidar -- 3 The Meteosat Images -- 4 Results -- 4.1 Overview -- 4.2 Strong Heterogeneity in the Cloud Layer -- 4.3 Dry Regions in Both Cloud and Sub-cloud Layers -- 4.4 Transport of Moisture Through the Cloud Layer by Shallow Convection -- 4.5 Mean, Variance and Skewness Profiles of Water Vapor -- 5 Conclusions and Outlook -- References -- 13 Emerging Technologies and Synergies for Airborne and Space-Based Measurements of Water Vapor Profiles -- 1 Introduction -- 2 Differential Absorption Lidar -- 2.1 Measurement Capabilities -- 2.2 Technology Readiness -- 3 Differential Absorption Radar -- 3.1 Measurement Capabilities -- 3.2 Technology Readiness -- 4 Microwave Occultation -- 4.1 Measurement Approach -- 4.2 Measurement Capabilities -- 4.3 Technology Readiness -- 5 Hyperspectral Microwave -- 5.1 Measurement Capabilities -- 5.2 Technology Readiness -- 6 Synergies of Observing Systems -- 6.1 Value of Ground-Based Profiling -- 6.2 Examples of Synergetic Applications -- 6.2.1 Combining Lidar and Microwave Radiometer -- 6.2.2 Combining Satellite and Ground-Based Observations -- 6.3 Future Perspectives -- 7 Summary and Conclusions -- References. , 14 Observational Constraints on Cloud Feedbacks: The Role of Active Satellite Sensors.
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  • 3
    Keywords: Forschungsbericht ; Klima ; Atmosphäre ; Prognose ; Modell
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (16 Seiten, 213,99 KB)
    Language: German
    Note: Förderkennzeichen BMBF 01LP1128A - 01LP1128B. - Verbund-Nummer 01098226 , Autoren dem Berichtsblatt entnommen , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Zusammenfassungen in deutscher und englischer Sprache
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  • 4
    Keywords: Forschungsbericht ; Klima ; Modell ; Wolke
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (5 Seiten, 143,31 KB)
    Language: German
    Note: Förderkennzeichen BMBF 01LK1201A , Im Titel ist "2" in HD(CP)2 hochgestellt , Autoren dem Berichtsblatt entnommen , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden , Mit deutscher und englischer Zusammenfassung
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  • 5
    Publication Date: 2023-12-05
    Description: Clouds are primary modulators of Earth's energy balance. It is thus important to understand the links connecting variabilities in cloudiness to variabilities in other state variables of the climate system, and also describe how these links would change in a changing climate. A conceptual model of global cloudiness can help elucidate these points. In this work we derive simple representations of cloudiness, that can be useful in creating a theory of global cloudiness. These representations illustrate how both spatial and temporal variability of cloudiness can be expressed in terms of basic state variables. Specifically, cloud albedo is captured by a nonlinear combination of pressure velocity and a measure of the low‐level stability, and cloud longwave effect is captured by surface temperature, pressure velocity, and standard deviation of pressure velocity. We conclude with a short discussion on the usefulness of this work in the context of global warming response studies.
    Description: Plain Language Summary: Clouds are important for Earth's climate, because they affect a large portion of the planet's energy balance, and hence its mean temperature. To better understand how the interplay between cloudiness and energy balance would change in a changing climate, a better theoretical understanding of how clouds are distributed over the planet, and how this connects with the state variables of the climate system such as temperature and wind speed, is required. As theoretical understanding is currently limited, in this work we explore the possibility of very simply representing the spatiotemporal distribution of clouds over the whole planet. We believe that these simple representations advance the field in the direction of a conceptual theory of global cloudiness and its impact on the energy balance. We show that the impact of cloudiness on both solar and terrestrial radiation balance can be captured well globally with only a few predictive fields, like surface temperature or vertical wind speed, combined simply and using only three tunable parameters, and without using any supplementary information such as the particular season or location on the planet.
    Description: Key Points: Model fits are performed to the spatiotemporal observed cloudiness over all oceans, using a minimal set of predictors and parameters. Models capture global‐mean, spatial, and most of seasonal variability of cloud radiative effects. Cloud albedo and longwave effect are captured by pressure velocity and its variance, surface temperature, and lower tropospheric stability.
    Description: CONSTRAIN project EU Horizon 2020
    Keywords: ddc:551.5 ; global cloudiness ; energy balance ; cloud controlling factors
    Language: English
    Type: doc-type:article
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  • 6
    Publication Date: 2022-10-06
    Description: Abundant rainfall over tropical land masses sustains rich ecosystems, a crucial source of biodiversity and sink of carbon. Here, we use two characteristics of the observed tropical precipitation distribution, its distinctive zonal arrangement and its partitioning between land and ocean, to understand whether land conditions the climate to receive more than its fair share of precipitation as set by the land‐sea distribution. Our analysis demonstrates that it is not possible to explain the tropics‐wide partitioning of precipitation unless one assumes that rain is favored over land. Land receives more than its fair share of precipitation by broadening and letting the tropical rainbelts move more, effectively underpinning a negative feedback between surface water storage and precipitation. In contrast, rain is disfavored over land in climate models. Our findings suggest that the abundance of rainfall that shapes the terrestrial tropical biosphere is more robust to perturbations than models have suggested.
    Description: Plain Language Summary: Many ecosystems depend on the presence of a land surface exposed to precipitation to exist and prosper. In contrast to the marine biota, though, the terrestrial biosphere cannot directly tap into an unlimited reservoir of water molecules that can be recycled to support life. Yet, observations indicate that it rains in mean 3 mm day−1 over tropical land and 3 mm day−1 over tropical ocean, giving the surprising impression that precipitation amounts are not altered by the presence of land. Investigating the factors controlling this tropics‐wide partitioning of precipitation, we show that geometrical constraints actually would lead to a precipitation ratio of 0.86, not 1.0, if the presence of land would not matter. Comparing this theoretical value to observations, we find that the land receives more than its fair share of precipitation. This happens by broadening and letting the tropical rainbelt moves more over land. By quantifying the strength of the land control on the tropics‐wide partitioning of precipitation, we can also deduce that a negative feedback exists between evapotranspiration and precipitation. In contrast, repeating the same analysis with climate models reveals a positive feedback, questioning the ability of climate models to simulate regional tropical precipitation changes.
    Description: Key Points: A conceptual model of tropical precipitation is derived to understand the tropics‐wide partitioning of precipitation between land and ocean. The size and location of continent constrain the tropical land‐to‐ocean precipitation ratio to lie between 0.74 and 0.95 with a mean of 0.86. Observed ratios from six data sets are larger than these values, indicating that land receives more than its fair share of precipitation.
    Description: http://hdl.handle.net/21.11116/0000-000A-1DEC-D
    Keywords: ddc:551.6
    Language: English
    Type: doc-type:article
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  • 7
    Publication Date: 2024-02-28
    Description: 〈title xmlns:mml="http://www.w3.org/1998/Math/MathML"〉Abstract〈/title〉〈p xmlns:mml="http://www.w3.org/1998/Math/MathML" xml:lang="en"〉Extremely high land surface temperatures affect soil ecological processes, alter land‐atmosphere interactions, and may limit some forms of life. Extreme surface temperature hotspots are presently identified using satellite observations or deduced from complex Earth system models. We introduce a simple, yet physically based analytical approach that incorporates salient land characteristics and atmospheric conditions to globally identify locations of extreme surface temperatures and their upper bounds. We then provide a predictive tool for delineating the spatial extent of land hotspots at the limits to biological adaptability. The model is in good agreement with satellite observations showing that temperature hotspots are associated with high radiation and low wind speed and occur primarily in Middle East and North Africa, with maximum temperatures exceeding 85°C during the study period from 2005 to 2020. We observed an increasing trend in maximum surface temperatures at a rate of 0.17°C/decade. The model allows quantifying how upper bounds of extreme temperatures can increase in a warming climate in the future for which we do not have satellite observations and offers new insights on potential impacts of future warming on limits to plant growth and biological adaptability.〈/p〉
    Description: Plain Language Summary: While satellite imagery can identify extreme land surface temperatures, land and atmospheric conditions for the onset of maximum land surface temperature (LST) have not yet been globally explored. We developed a physically based analytical model for quantifying the value and spatial extent of maximum LST and provide insights into combinations of land and atmospheric conditions for the onset of such temperature extremes. Results show that extreme LST hotspots occur primarily in the Middle East and North Africa with highest values near 85°C. Importantly, persistence of surface temperatures exceeding 75°C limits vegetation growth and disrupts primary productivity such as in Lut desert in Iran. The study shows that with global warming, regions with prohibitive land surface temperatures will expand.〈/p〉
    Description: Key Points: 〈list list-type="bullet"〉 〈list-item〉 〈p xml:lang="en"〉Hotspots for high land surface temperatures (LSTs) were globally identified using a physically based analytical approach incorporating land and atmospheric conditions〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉High LSTs primarily occur in Middle East and North Africa with values exceeding 85°C〈/p〉〈/list-item〉 〈list-item〉 〈p xml:lang="en"〉Maximum LSTs rising at a rate of 0.17°C/decade may limit plant growth and biological adaptability in a warming world〈/p〉〈/list-item〉 〈/list〉 〈/p〉
    Description: Hamburg University of Technology
    Description: European Union's Horizon Europe Research and Innovation Programme
    Description: https://disc.gsfc.nasa.gov/datasets/M2I1NXLFO_5.12.4/summary
    Description: https://disc.gsfc.nasa.gov/datasets/M2T1NXRAD_5.12.4/summary
    Description: https://doi.org/10.5067/MODIS/MCD12C1.006
    Description: https://doi.org/10.3133/ofr20111073
    Description: https://www.nccs.nasa.gov/services/data-collections/land-based-products/nex-gddp-cmip6
    Description: https://doi.org/10.3334/ORNLDAAC/1247
    Keywords: ddc:551.5 ; maximum land surface temperature (LST) ; land conditions ; atmospheric conditions ; LST hotspots
    Language: English
    Type: doc-type:article
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  • 8
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Earth and Planetary Sciences 33 (2005), S. 605-643 
    ISSN: 0084-6597
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Geosciences , Physics
    Notes: Various forms of atmospheric moist convection are reviewed through a consideration of three prevalent regimes: stratocumulus; trade-wind; and deep, precipitating, maritime convection. These regimes are chosen because they are structural components of the general circulation of the atmosphere and because they highlight distinguishing features of this polymorphous phenomenon. In particular, the ways in which varied forms of moist convection communicate with remote parts of the flow through mechanisms other than the rearrangement of fluid parcels are emphasized. These include radiative, gravity wave, and/or microphysical (precipitation) processes. For each regime, basic aspects of its phenomenology are presented along with theoretical frameworks that have arisen to help rationalize the phenomenology. Recent developments suggest that the increased capacity for numerical simulation and increasingly refined remote sensing capabilities bodes well for major advances in the coming years.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1573-1472
    Keywords: Cloud-topped boundary layers ; Stratocumulus ; Drizzle ; Cloud-radiation feedback ; Entrainment ; Large-eddy simulation
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences , Physics
    Notes: Abstract Three single-column models (all with an explicit liquid water budget and compara-tively high vertical resolution) and three two-dimensional eddy-resolving models (including one with bin-resolved microphysics) are compared with observations from the first ASTEX Lagrangian experiment. This intercomparison was a part of the second GCSS boundary-layer cloud modelling workshop in August 1995. In the air column tracked during the first ASTEX Lagrangian experiment, a shallow subtropical drizzling stratocumulus-capped marine boundary layer deepens after two days into a cumulus capped boundary layer with patchy stratocumulus. The models are forced with time varying boundary conditions at the sea-surface and the capping inversion to simulate the changing environment of the air column. The models all predict the observed deepening and decoupling of the boundary layer quite well, with cumulus cloud evolution and thinning of the overlying stratocumulus. Thus these models all appear capable of predicting transitions between cloud and boundary-layer types with some skill. The models also produce realistic drizzle rates, but there are substantial quantitative differences in the cloud cover and liquid water path between models. The differences between the eddy-resolving model results are nearly as large as between the single column model results. The eddy resolving models give a more detailed picture of the boundary-layer evolution than the single-column models, but are still sensitive to the choice of microphysical and radiative parameterizations, sub-grid-scale turbulence models, and probably model resolution and dimensionality. One important example of the differences seen in these parameterizations is the absorption of solar radiation in a specified cloud layer, which varied by a factor of four between the model radiation parameterizations.
    Type of Medium: Electronic Resource
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  • 10
    Publication Date: 2021-07-04
    Description: In order to enhance our understanding of clouds and their microphysical processes, it is crucial to exploit both observations and models. Local observations from ground‐based remote sensing sites provide detailed information on clouds, but as they are limited in dimension, there is no straightforward way to use them to guide large‐scale model development. We show that large‐eddy simulations (LES) performed on similar temporal and spatial scales as the local observations can bridge this gap. Recently, LES with realistic topography and lateral boundary conditions became feasible for domains spanning several 100 km. In this study, we show how these simulations can be linked to observations of the Jülich Observatory for Cloud Evolution (JOYCE) for a 9‐day period in spring 2013. We discuss the advantages and disadvantages of very large versus small but more constrained domains as well as the differences compared to more idealized setups. The semi‐idealized LES include time‐varying forcing but are run with homogeneous surfaces and periodic boundary conditions. These assumptions seem to be the reason why they struggle to represent the observed varying conditions. The simulations using the “realistic” setup are able to represent the general cloud structure (timing, height, phase). It seems that the smaller and more constrained domain allows for a tighter control on the synoptic situation and is the preferred choice to ensure the comparability to the local observations. These simulations together with measures as the shown Hellinger distance will allow us to gain more insights into the representativeness of column measurements in the future.
    Description: Plain Language Summary: Clouds are still a cause for uncertainty in our understanding of climate and climate feedbacks. Due to the large range of involved scales—from small droplets up to storm systems—their representation in weather and climate models is an ongoing challenge. While new and sophisticated measurements of the atmospheric column could provide new insights into important processes, their linking to models is not trivial and is ongoing research. In this study, we are presenting and exploring different approaches to combine local observations of clouds with state‐of‐the‐art high‐resolution simulations. And we are presenting a setup, which shows a promising representation of the observed clouds and is constrained enough to be applicable for long‐term statistics—one of the key requirements for improvements and evaluation clouds in of weather and climate models.
    Description: Key Points: Large‐eddy simulations including external variability can bridge the gap between ground‐based observations of clouds and large‐scale models. For comparison with local observations, it is important to take external variability (e.g., large‐scale forcing and surface) into account. ICON‐LEM offers new possibilities to simulate small scales while considering external variability.
    Keywords: 551.5 ; clouds ; heterogeneity ; ICON‐LEM ; large‐scale forcing ; LES ; remote sensing
    Type: article
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