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  • 1
    Keywords: Earth sciences. ; Electronic books.
    Type of Medium: Online Resource
    Pages: 1 online resource (242 pages)
    Edition: 1st ed.
    ISBN: 9783319138657
    Series Statement: Springer Earth System Sciences Series
    DDC: 363.73874
    Language: English
    Note: Intro -- Acknowledgments -- Contents -- Part I Introduction -- 1 Earth System Science---Past Experiences and Future Trends -- Abstract -- 1 Introduction -- 2 Review -- 3 Future Trends -- 4 Conclusion -- References -- 2 The Educational Program of the Earth System Science Research School (ESSReS) -- Abstract -- 1 Introduction -- 2 The Educational Program -- 2.1 Introductory Courses -- 2.2 Expert Courses -- 2.3 Seminar Series -- 2.4 Computational Skills Courses -- 2.5 Transferable Skill Courses -- 2.6 Academic Writing Courses -- 2.7 Excursions -- 2.8 Annual Retreat -- 3 International Exchange -- 3.1 International and National Meetings -- 3.2 Visit in a Foreign Lab -- 3.3 Invited Guest Scientists -- 4 Progress Assessments -- 5 Conclusions -- References -- 3 Time Evolution of a PhD Student's Mood---A Review of My Time as PhD Student of the Research School ESSReS -- 1 Introduction -- 2 Time Evolution of a PhD Students's Mood -- 3 Conclusion -- References -- 4 Progress in Earth System Science: What Does It Take to Make Our Ideas Clear? -- Abstract -- 1 Self-critical Approach -- 2 Hypothesis Testing and Models -- 3 Building of Models and Expressing the Scientific Discoveries -- References -- Part II Remote Sensing and Modelling of Atmospheric Chemistry and Sea Ice Parameters -- 5 Towards a Better Tropospheric Ozone Data Product from SCIAMACHY: Improvements in High Latitude Stratospheric Ozone -- Abstract -- 1 Introduction -- 2 Limb Measurements and Comparison Methodology -- 3 SCIAMACHY Limb Retrieval of Version 2.9 -- 4 SCIAMACHY Limb Retrieval of Version 3.0 and Comparison Results -- 5 Conclusions -- Acknowledgments -- References -- 6 Ten-Year SCIAMACHY Stratospheric Aerosol Data Record: Signature of the Secondary Meridional Circulation Associated with the Quasi-Biennial Oscillation -- Abstract -- 1 Introduction -- 2 Instrument and Data. , 3 Results and Discussion -- 4 Conclusions -- Acknowledgments -- References -- 7 Investigating the Link Between Glyoxal and Biogenic Activities -- Abstract -- 1 Introduction -- 2 Glyoxal Retrieval -- 3 Results and Discussion -- 4 Conclusions -- Acknowledgments -- References -- 8 Estimates of NOx Emission Factors from GOME-2 Measurements for the Major Types of Open Biomass Burning -- Abstract -- 1 Introduction -- 2 Data and Methods -- 2.1 Satellite Measurements of TVC NO2 -- 2.2 Satellite Measurements of FRP -- 2.3 Land Cover Type Product -- 2.4 Production Rate of NOx from Fire -- 2.5 Estimation of NOx Emission Factors -- 3 Results and Discussion -- 4 Conclusions and Outlook -- References -- 9 The Use of FTIR-Spectrometry in Combination with Different Biosphere-Atmosphere Flux Measurement Techniques -- Abstract -- 1 Introduction -- 2 Experimental Setup -- 2.1 The Flux Gradient Technique -- 2.2 The Flux Chamber Technique -- 3 Flux Gradient- and Flux Chamber Measurements -- 4 Discussion and Conclusion -- Acknowledgments -- References -- 10 Near-Infrared Lunar Absorption Spectroscopy for the Retrieval of Column Averaged CO2 and CH4 -- Abstract -- 1 Introduction -- 2 Ground-Based Column Averaged Trace Gas Retrieval -- 3 Spectra from the Bremen Instrument Setup -- 4 xCO2 and xCH4 from Lunar Absorption Spectroscopy -- 5 Conclusions -- Acknowledgements -- References -- 11 A New Method to Filter Out Radio-Frequency Interference (RFI) from SMOS Level 1C Data for Sea Ice Applications -- Abstract -- 1 Introduction -- 2 Data Description -- 3 Filtering Procedure -- 4 Conclusion -- Acknowledgments -- References -- 12 Arctic Multiyear Ice Concentration Retrieval from SSM/I Data Using the NASA Team Algorithm with Dynamic Tie Points -- Abstract -- 1 Introduction -- 2 Method -- 3 Time Series Results -- 4 Sensitivity Study and Conclusion -- Acknowledgements -- References. , 13 Detecting CDOM Fluorescence Using High Spectrally Resolved Satellite Data: A Model Study -- Abstract -- 1 Introduction -- 2 Methods -- 2.1 DOAS Retrieval Technique -- 2.2 CDOM Fluorescence Modeling -- 2.2.1 CDOM as Mixture of Humic and Fulvic Acids -- 2.2.2 Excitation-Emission Matrices Approach -- 3 Results and Discussion -- 4 Conclusions and Outlook -- Acknowledgments -- References -- Part III Physical Oceanography -- 14 The Flow of Dense Water Plumes in the Western Weddell Sea Simulated with the Finite Element Ocean Model (FEOM) -- Abstract -- 1 Introduction -- 2 Model Setup and Experiments -- 3 Results -- 4 Summary and Conclusions -- Acknowledgments -- References -- 15 Data Analysis and Modeling of the Amundsen Sea Embayment -- Abstract -- 1 Introduction -- 2 Hydrographic Data Analysis -- 3 Modeling of the Amundsen Sea -- 4 Discussion and Outlook -- References -- Part IV Sea-ice Physics -- 16 Impact of Sea-Ice Bottom Topography on the Ekman Pumping -- Abstract -- 1 Introduction -- 2 Data and Methods -- 3 Calculation of Oceanic Drag Coefficients -- 4 Ekman Pumping -- 5 Summary and Conclusion -- Acknowledgments -- References -- 17 Classification of CryoSat-2 Radar Echoes -- Abstract -- 1 Introduction -- 2 Methods -- 3 Results -- 4 Discussion -- 5 Conclusion -- Acknowledgments -- References -- Part V Earth System Modelling and Data Analysis -- 18 Integration of Passive Tracers in a Three-Dimensional Ice Sheet Model -- Abstract -- 1 Introduction -- 2 Methods -- 2.1 Present Day Control Run -- 2.2 Passive Tracer Advection -- 2.2.1 Validation of Tracer Modules -- 2.2.2 Analytical Comparison to the Nye-Vialov Solution -- 3 Discussion -- References -- Part VI Climate Archives and Geotectonics -- 19 Bivalve Shells---Unique High-Resolution Archives of the Environmental Past -- Abstract -- 1 Introduction -- 2 Methods -- 2.1 Shell Origin and Laboratory Work. , 2.2 State of Preservation -- 2.3 Frequency Analysis -- 2.4 Stable Oxygen Isotopes ( delta 18O) -- 3 Results -- 3.1 State of Preservation -- 3.2 Frequency Analysis -- 3.3 Stable Oxygen Isotopes ( delta 18O) -- 4 Discussion and Conclusions -- Acknowledgments -- References -- 20 Functional Diversity and Traits Assembly Patterns of Benthic Macrofaunal Communities in the Southern North Sea -- Abstract -- 1 Introduction -- 2 Material and Methods -- 3 Results -- 4 Discussion -- Acknowledgments -- 21 Snow Accumulation in North Greenland over the Last Millennium -- Abstract -- 1 Introduction -- 2 Methods -- 3 Results -- 4 Discussion and Conclusion -- References -- 22 Seismostratigraphic Analysis and Glacial History of the Weddell Sea Region, Antarctica -- Abstract -- 1 Introduction -- 2 Data and Methods -- 3 Results -- 3.1 Seismic Characteristics and Horizon Stratigraphy -- 3.2 Sedimentation Rates -- 4 Discussion and Conclusions -- Acknowledgments -- References -- Part VII Geoinformatics -- 23 Visual Analysis of Relevant Fields in Geoscientific Multifield Data -- Abstract -- 1 Introduction -- 2 Related Work -- 3 Field Similarity Plot -- 4 Interactive Visual Analysis -- 5 Use Cases -- 5.1 Multifield -- 5.2 Time-Varying Field -- 6 Discussion -- 7 Conclusion -- Acknowledgements -- References -- 24 A Database Language More Suitable for the Earth System Sciences -- Abstract -- 1 Introduction -- 2 Data Model -- 3 Query Language -- 3.1 Array Construction -- 3.2 Array Inspection Operators -- 3.3 Array Aggregation -- 3.4 Derived Operators -- 3.5 Array \leftrightarrow Table Conversion -- 3.6 Array \leftrightarrow LOB Conversion -- 4 Implementation -- 5 Conclusion -- Acknowledgments -- References -- 25 Towards Collaborative Exploration and Analysis of Big Data from Mars: A Noachis Terra Case Study -- Abstract -- 1 Introduction -- 2 Data and Methods. , 3 Noachis Terra Case Study -- 4 Discussion -- 5 Conclusions -- Acknowledgments -- References.
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  • 2
    Keywords: Earth System Sciences ; Physical geography. ; Atmospheric sciences. ; Geography
    Description / Table of Contents: 1 Earth System Science - past experiences and future trends -- 2 The educational program of the Earth System Science Research School (ESSReS) -- 3 Time evolution of a PhD student's mood - A review of my time as PhD student in the research school ESSReS -- 4 Progress in Earth System Science: What does it take to make our ideas clear -- 5 Towards a better tropospheric ozone product from SCIAMACHY: improvements in high latitude stratospheric ozone -- 6 Ten-year SCIAMACHY Stratospheric Aerosol data record: Signature of the Secondary Meridional Circulation associated with the Quasi-Biennial Oscillation in the Tropical Stratosphere -- 7 Investigating the link between glyoxal and biogenic activities -- 8 Estimates of NOx emission factors from GOME-2 measurements for the major types of open biomass burning -- 9 The use of FTIR-spectrometry in combination with different biosphere-atmosphere flux measurement techniques -- 10 Near-infrared lunar absorption spectroscopy for the retrieval of column averaged CO2 and CH4 -- 11 A new method to filter out radio-frequency interference (RFI) from SMOS level 1C data for sea ice applications -- 12 Arctic Multiyear Ice Concentration Retrieval from SSM/I data using the NASA Team algorithm with dynamic tie points -- 13 Detecting CDOM fluorescence using high spectrally resolved satellite data: a model study -- 14 The flow of dense water plumes in the western Weddell Sea simulated with the Finite Element Ocean Model (FEOM) -- 15 Data analysis and modeling of the Amundsen Sea embayment -- 16 Impact of sea-ice bottom topography on the Ekman pumping -- 17 Classification of CryoSat-2 radar echoes -- 18 Integration of passive tracers in a three-dimensional ice sheet model -- 19 Bivalve shells - unique high-resolution archives of environmental past -- 20 Functional diversity and traits assembly patterns of benthic macrofaunal communities in the southern North Sea -- 21 Snow accumulation in North Greenland over the last millennium -- 22 Seismostratigraphic analysis and glacial history of the Weddell Sea region, Antarctica -- 23 Visual analysis of Relevant Fields in Geoscientific Multifield Data -- 24 A Database Language Suitable for the Earth System Sciences -- 25 Towards Collaborative Exploration and Analysis of Big Data from Mars: A Noachis Terra Case Study
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (X, 251 p. 86 illus., 83 illus. in color)
    Edition: 1st ed. 2015
    ISBN: 9783319138657
    Series Statement: Springer Earth System Sciences
    Language: English
    Note: Description based upon print version of record , 1 Earth System Science - past experiences and future trends2 The educational program of the Earth System Science Research School (ESSReS) -- 3 Time evolution of a PhD student's mood - A review of my time as PhD student in the research school ESSReS -- 4 Progress in Earth System Science: What does it take to make our ideas clear -- 5 Towards a better tropospheric ozone product from SCIAMACHY: improvements in high latitude stratospheric ozone -- 6 Ten-year SCIAMACHY Stratospheric Aerosol data record: Signature of the Secondary Meridional Circulation associated with the Quasi-Biennial Oscillation in the Tropical Stratosphere -- 7 Investigating the link between glyoxal and biogenic activities -- 8 Estimates of NOx emission factors from GOME-2 measurements for the major types of open biomass burning -- 9 The use of FTIR-spectrometry in combination with different biosphere-atmosphere flux measurement techniques -- 10 Near-infrared lunar absorption spectroscopy for the retrieval of column averaged CO2 and CH4 -- 11 A new method to filter out radio-frequency interference (RFI) from SMOS level 1C data for sea ice applications -- 12 Arctic Multiyear Ice Concentration Retrieval from SSM/I data using the NASA Team algorithm with dynamic tie points -- 13 Detecting CDOM fluorescence using high spectrally resolved satellite data: a model study -- 14 The flow of dense water plumes in the western Weddell Sea simulated with the Finite Element Ocean Model (FEOM) -- 15 Data analysis and modeling of the Amundsen Sea embayment -- 16 Impact of sea-ice bottom topography on the Ekman pumping -- 17 Classification of CryoSat-2 radar echoes -- 18 Integration of passive tracers in a three-dimensional ice sheet model -- 19 Bivalve shells - unique high-resolution archives of environmental past -- 20 Functional diversity and traits assembly patterns of benthic macrofaunal communities in the southern North Sea -- 21 Snow accumulation in North Greenland over the last millennium -- 22 Seismostratigraphic analysis and glacial history of the Weddell Sea region, Antarctica -- 23 Visual analysis of Relevant Fields in Geoscientific Multifield Data -- 24 A Database Language Suitable for the Earth System Sciences -- 25 Towards Collaborative Exploration and Analysis of Big Data from Mars: A Noachis Terra Case Study.
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  • 3
    Publication Date: 2019-02-01
    Description: Estuaries are sources of nitrous oxide (N2O) and methane (CH4) to the atmosphere. However, our present knowledge of N2O and CH4 emissions from estuaries in the tropics is very limited because data are scarce. In this study, we present first measurements of dissolved N2O and CH4 from two estuaries in a peat-dominated region of northwestern Borneo. Two campaigns (during the dry season in June 2013 and during the wet season in March 2014) were conducted in the estuaries of the Lupar and Saribas rivers. Median N2O concentrations ranged between 7.2 and 12.3 nmol L−1 and were higher in the marine end-member (13.0 ± 7.0 nmol L−1). CH4 concentrations were low in the coastal ocean (3.6 ± 0.2 nmol L−1) and higher in the estuaries (medians between 10.6 and 64.0 nmol L−1). The respiration of abundant organic matter and presumably anthropogenic input caused slight eutrophication, which did not lead to hypoxia or enhanced N2O concentrations, however. Generally, N2O concentrations were not related to dissolved inorganic nitrogen concentrations. Thus, the use of an emission factor for the calculation of N2O emissions from the inorganic nitrogen load leads to an overestimation of the flux from the Lupar and Saribas estuaries. N2O was negatively correlated with salinity during the dry season, which suggests a riverine source. In contrast, N2O concentrations during the wet season were not correlated with salinity but locally enhanced within the estuaries, implying that there were additional estuarine sources during the wet (i.e., monsoon) season. Estuarine CH4 distributions were not driven by freshwater input but rather by tidal variations. Both N2O and CH4 concentrations were more variable during the wet season. We infer that the wet season dominates the variability of the N2O and CH4 concentrations and subsequent emissions from tropical estuaries. Thus, we speculate that any changes in the Southeast Asian monsoon system will lead to changes in the N2O and CH4 emissions from these systems. We also suggest that the ongoing cultivation of peat soil in Borneo is likely to increase N2O emissions from these estuaries, while the effect on CH4 remains uncertain.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
    Format: text
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  • 4
    Publication Date: 2019-09-23
    Description: Interest in stratospheric aerosol and its role in climate have increased over the last decade due to the observed increase in stratospheric aerosol since 2000 and the potential for changes in the sulfur cycle induced by climate change. This review provides an overview about the advances in stratospheric aerosol research since the last comprehensive assessment of stratospheric aerosol was published in 2006. A crucial development since 2006 is the substantial improvement in the agreement between in situ and space-based inferences of stratospheric aerosol properties during volcanically quiescent periods. Furthermore, new measurement systems and techniques, both in situ and space based, have been developed for measuring physical aerosol properties with greater accuracy and for characterizing aerosol composition. However, these changes induce challenges to constructing a long-term stratospheric aerosol climatology. Currently, changes in stratospheric aerosol levels less than 20% cannot be confidently quantified. The volcanic signals tend to mask any nonvolcanically driven change, making them difficult to understand. While the role of carbonyl sulfide as a substantial and relatively constant source of stratospheric sulfur has been confirmed by new observations and model simulations, large uncertainties remain with respect to the contribution from anthropogenic sulfur dioxide emissions. New evidence has been provided that stratospheric aerosol can also contain small amounts of nonsulfate matter such as black carbon and organics. Chemistry-climate models have substantially increased in quantity and sophistication. In many models the implementation of stratospheric aerosol processes is coupled to radiation and/or stratospheric chemistry modules to account for relevant feedback processes
    Type: Article , PeerReviewed
    Format: text
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  • 5
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    In:  Supplement to: Buschmann, Matthias; Deutscher, Nicholas M; Palm, Mathias; Warneke, Thorsten; Weinzierl, Christine; Notholt, Justus (2017): The arctic seasonal cycle of total column CO2 and CH4 from ground-based solar and lunar FTIR absorption spectrometry. Atmospheric Measurement Techniques, 10(7), 2397-2411, https://doi.org/10.5194/amt-10-2397-2017
    Publication Date: 2023-10-28
    Description: At the Ny-Ålesund TCCON site, solar and lunar Fourier-Transform InfraRed (FTIR) absorption spectroscopy is performed to retrieve the column averaged dry-air mole fractions of various trace gases. In this data set, daily averages of the TCCON solar absorption measurements and nightly averages of lunar absorption measurements of xCO2 and xCH4 are provided. As an indication of the error of the measurement, the standard deviation of the daily mean and the number of contributing measurements are presented as well.
    Keywords: AC3; Arctic Amplification; Carbon dioxide, dry-air mole fraction; Carbon dioxide, dry-air mole fraction, standard deviation; Comment; DATE/TIME; Fourier transform infrared absorption spectroscopy (FTIR); Methane, dry-air mole fraction; Methane, dry-air mole fraction, standard deviation; Monitoring station; MONS; Number of observations; NYA_TCCON; Ny-Ålesund, Spitsbergen
    Type: Dataset
    Format: text/tab-separated-values, 2037 data points
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  • 6
    Publication Date: 2024-01-24
    Description: CO2 is the strongest anthropogenic forcing agent for climate change since pre-industrial times. Like other greenhouse gases, CO2 absorbs terrestrial surface radiation and causes emission from the atmosphere to space. As the surface is generally warmer than the atmosphere, the total long-wave emission to space is commonly less than the surface emission. However, this does not hold true for the high elevated areas of central Antarctica. For this region, the emission to space is higher than the surface emission; and the greenhouse effect of CO2 is around zero or even negative, which has not been discussed so far. We investigated this in detail and show that for central Antarctica an increase in CO2 concentration leads to an increased long-wave energy loss to space, which cools the Earth-atmosphere system. These findings for central Antarctica are in contrast to the general warming effect of increasing CO2.
    Keywords: Antarctica; Baseline Surface Radiation Network; BSRN; Monitoring station; MONS; South Pole; SPO
    Type: Dataset
    Format: 226 datasets
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  • 7
    Publication Date: 2024-04-20
    Description: During the legs PS106 and PS107 of the RV Polarstern, a Fourier-Transform Infrared (FTIR) spectrometer was used to measure radiation emitted by clouds. Spectra were recorded between 700 cm^-1 (14.29 micrometer) and 1200 cm^-1 (8.33 micrometer). From these spectra, the cloud optical depths and the effective droplet radii were retrieved and the liquid water path (LWP), ice water path (IWP) and the condensed water path (CWP=IWP+LWP) calculated. The errors of the cloud optical depths and the effective droplet radii are the standard deviations of the retrieval, from which the errors of LWP, IWP and CWP were calculated. The averaging kernel matrices describe the sensitivity of the retrieval to the parameters. Cloud base heights were taken from the Polarstern ceilometer CL51. See also: Ceilometer CL51 raw data: https://doi.pangaea.de/10.1594/PANGAEA.883320 https://doi.pangaea.de/10.1594/PANGAEA.883322 https://doi.pangaea.de/10.1594/PANGAEA.883323
    Keywords: AC3; Arctic; Arctic Amplification; ARK-XXXI/1.1,PASCAL; ARK-XXXI/1.2; ARK-XXXI/2; clouds; Event label; File format; File name; File size; Fourier Transform Infrared Radiometer; FTIR; Polarstern; PS106_0_Underway-13; PS106/1; PS106/2; PS106/2_0_Underway-1; PS107; PS107_0_underway-16; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 8
    Publication Date: 2024-04-20
    Description: In summer 2017, measurements of atmospheric radiance were performed using a mobile emission Fourier Transform Infrared (EM-FTIR) spectrometer. This EM-FTIR spectrometer was carried by the RV Polarstern. Retrievals of cloud parameters were performed from radiance measurements from the 11th of June 2017 until the 11th August 2017 in the Arctic Ocean around Svalbard and the Fram Strait. This dataset contains retrieved cloud optical depths of liquid water and ice water, effective radii of liquid water droplets and ice crystals. From these, the liquid water paths and ice water paths are calculated. The retrieval of microphysical cloud parameters uses spectral radiances between 500cm^-1 and 1200 cm^-1. Retrieval has been done using the Total Cloud Water retrieval (TCWret): https://doi.org/10.5281/ZENODO.4621127 Cloud heights were taken from the Ceilometer CL51, located on the RV Polarstern. Data can be found here: https://doi.pangaea.de/10.1594/PANGAEA.883320 https://doi.pangaea.de/10.1594/PANGAEA.883322 https://doi.pangaea.de/10.1594/PANGAEA.883323
    Keywords: AC3; Arctic; Arctic Amplification; ARK-XXXI/1.1,PASCAL; ARK-XXXI/1.2; ARK-XXXI/2; clouds; Fourier Transform Infrared Radiometer; FTIR; Polarstern; PS106_0_Underway-13; PS106/1; PS106/2; PS106/2_0_Underway-1; PS107; PS107_0_underway-16
    Type: Dataset
    Format: application/x-hdf, 17.9 MBytes
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  • 9
    Publication Date: 2019-06-17
    Description: Clouds play an important role in Arctic amplification. This term represents the recently observed enhanced warming of the Arctic relative to the global increase of near-surface air temperature. However, there are still important knowledge gaps regarding the interplay between Arctic clouds and aerosol particles, and surface properties, as well as turbulent and radiative fluxes that inhibit accurate model simulations of clouds in the Arctic climate system. In an attempt to resolve this so-called Arctic cloud puzzle, two comprehensive and closely coordinated field studies were conducted: the Arctic Cloud Observations Using Airborne Measurements during Polar Day (ACLOUD) aircraft campaign and the Physical Feedbacks of Arctic Boundary Layer, Sea Ice, Cloud and Aerosol (PASCAL) ice breaker expedition. Both observational studies were performed in the framework of the German Arctic Amplification: Climate Relevant Atmospheric and Surface Processes, and Feedback Mechanisms (AC)3 project. They took place in the vicinity of Svalbard, Norway, in May and June 2017. ACLOUD and PASCAL explored four pieces of the Arctic cloud puzzle: cloud properties, aerosol impact on clouds, atmospheric radiation, and turbulent dynamical processes. The two instrumented Polar 5 and Polar 6 aircraft; the icebreaker Research Vessel (R/V) Polarstern; an ice floe camp including an instrumented tethered balloon; and the permanent ground-based measurement station at Ny-Ålesund, Svalbard, were employed to observe Arctic low- and mid-level mixed-phase clouds and to investigate related atmospheric and surface processes. The Polar 5 aircraft served as a remote sensing observatory examining the clouds from above by downward-looking sensors; the Polar 6 aircraft operated as a flying in situ measurement laboratory sampling inside and below the clouds. Most of the collocated Polar 5/6 flights were conducted either above the R/V Polarstern or over the Ny-Ålesund station, both of which monitored the clouds from below using similar but upward-looking remote sensing techniques as the Polar 5 aircraft. Several of the flights were carried out underneath collocated satellite tracks. The paper motivates the scientific objectives of the ACLOUD/PASCAL observations and describes the measured quantities, retrieved parameters, and the applied complementary instrumentation. Furthermore, it discusses selected measurement results and poses critical research questions to be answered in future papers analyzing the data from the two field campaigns.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 10
    Publication Date: 2017-10-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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