Get a list of Observation objects.

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            "abstract": "The Chilbolton Observatory, Hampshire, have had a Vaisala CT75K lidar ceilometer deployed since 13th September 1996. This dataset contains measurements of the range of first, second, and third cloud base from the lidar and attenuated backscatter coefficients of aerosols within the atmosphere. Plots of the attenuated backscatter coefficient at different heights are also available.\r\n\r\nThe instrument has been regularly calibrated using the method described by O'Connor, Ewan J., Anthony J. Illingworth, Robin J. Hogan, 2004: A Technique for Auto-calibration of Cloud Lidar. J. Atmos. Oceanic Technol., 21, 777–786. doi: http://dx.doi.org/10.1175/1520-0426(2004)021<0777:ATFAOC>2.0.CO;2 . \r\n\r\nPrior to April 2014 this technique had been applied manually, but from 2014 this was automated to provide a routine, automated application of O'Connor et al's calibration technique. This also highlighted an instrument calibration drift not previously spotted in earlier data and so a corrected data have been added to the archive for the following periods (denoted by \"_cor1\" in the filename): 1st July 2003 – 31st December 2003, January 2006 to December 2012 and February and March 2013. Users should see the data quality notes for further details.\r\n\r\nThis dataset incorporates the earlier published and citable 1996 - 2013 collection of lidar data, but continues this dataset to present",
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            "title": "Global Vegetation Height Frequency Distributions (v1.1) from the ICESAT GLAS instrument produced under NCEO",
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                "abstract": "This vegetation height frequency distribution dataset was derived from data from the Geoscience Laser Altimeter System (GLAS) on the Ice, Cloud and land Elevation Satellite (ICESat), with data available from the NSIDC (nsidc.org)\r\n\r\nICESAT Geoscience Laser Altimeter System (GLAS) waveform data contain information on topography (slope) and objects on the surface (mostly vegetation). GLAS emits a laser pulse that is absorbed scattered and reflected by vegetation and the land surface. Vegetation height is derived from the GLA14 product release 31. This product contains the decomposition of waveforms in up to 6 Gaussians. Height is estimated from the difference between the first return, indicative of the top of the vegetation canopy or object, and the ground return. Ground return is estimated from the lowest of the two gaussians. The Gaussian with maximum amplitude of the last two Gaussians is thought to represent the ground return (Rosette et al. 2008). \r\n\r\nSpurious data were eliminated by applying a set of filters. Filters test for slope, difference in elevation between the wave form and the ground (indicative of clouds) and signal strength. An adjustment is applied for the shape of the last Gaussian.  Further details can be found in Los et al 2012."
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                    "abstract": "How feasible is it to predict Arctic climate at seasonal-to-interannual timescales? As part of the APPOSITE project a multi-model ensemble prediction experiment was conducted in order to answer this question.\r\n\r\nThe main goal of APPOSITE was to quantify the timescales on which Arctic climate is predictable. In order to achieve this, a coordinated set of idealised initial condition predictability experiments with seven general circulation models was conducted. This was the first intercomparison project designed to quantify the predictability of Arctic climate on seasonal to interannual timescales.\r\n\r\nSeveral different coupled climate models performed simulations for APPOSITE (see Doc below for Details of simulations submitted to the APPOSITE database). Six of these models followed the same experimental protocol (see Doc below for Control Simulations details and for Ensemble Predictions). One model, CanCM4 followed a slightly different protocol.\r\n\r\nThe Model data output from the APPOSITE project are now archived at CEDA. The collection of model outputs (control and prediction) include data from:\r\n\r\n- Canadian Centre for Climate Modelling and Analysis (CanCM4)\r\n- ECHAM6-FESOM (E6F), run and developed by the Alfred Wegener Institute.\r\n- EC-Earth consortium (ec-earth_v2_3)  \r\n- Geophysical Fluid Dynamics Laboratory (gfdlcm3)  \r\n- Met Office (hadgem1-2)  \r\n- Model for Interdisciplinary Research on Climate (MIROC5-2)  \r\n- Max-Planck-Institut for Meteorologie (mpiesm)\r\n\r\nAlthough designed to address Arctic predictability, this data set could also be used to assess the predictability of other regions and modes of climate variability on these timescales, such as the El Nino Southern Oscillation.\r\n\r\nA paper describing the simulations for APPOSITE is in preparation to be submitted to the Geoscientific Model Development Journal.\r\n\r\nNote: These data do not correspond to a particular time period since the studies are all conducted in the model world. They are not predictions or attempts to simulate a particular period of time. So the dates in the files are completely arbitrary. "
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                    "abstract": "This project was funded by the Natural Environment Research Council (NERC) with the grant reference - NE/K016008/1 - led by Professor Mathew Evans (University of York).\r\n\r\nClimate change and air pollution are two of the biggest challenges facing humanity today. Ozone and particulate matter are pollutants that are particularly harmful to human health. Recent studies have suggested that in the UK alone they cause 50,000 extra deaths and result in a financial burden of 8-22 billion pounds per year. Both ozone and particulate matter also play an important role in climate change. Ozone absorbs infra-red radiation resulting in a warming of the climate. Particles scatter and absorb incoming solar radiation and alter the properties of clouds. This results in complex interactions with the Earth's climate, with some types of aerosol pollution warming climate whereas others cool climate. Future air quality depends both on changes to emissions of pollutants and to changes in climate. Furthermore, a warming climate can result in worsened air pollution, which in turn can drive additional warming, meaning that complex feedbacks are possible between air pollution and climate.\r\n\r\nTo help understand these complex interactions and feedbacks scientists have developed Earth System Models that include a description of the important physical and biogeochemical processes. These models are increasingly being used by policy makers to make predictions about future air quality and climate and to guide policy decisions. It is therefore important that the models are rigorously tested. \r\n\r\nThis testing involves using detailed observations of atmospheric composition that have been made over the past few decades at locations around the world. Most model evaluation to date has involved testing whether the models simulate current average concentrations of atmospheric pollutants. Whilst this is a useful and necessary first step in model evaluation it does not test whether the model accurately simulates the change in concentration of a pollutant under changing emissions or changing climate. For example, does the model capture the real-world change in concentrations of a pollutant given a particular change in emission or under a future climate change scenario? This is particularly important as these predictions under-pin policy recommendations for air quality abatement. \r\n\r\nThis project synthesised long-term (multi-decadal) observations of ozone and particulate matter and their atmospheric precursors. They used these observations to explore trends and variability that have been observed over the past few decades. A model-observation framework was developed that can be used to evaluate how well models simulate observed variability and trends. The project tested state-of-the-art Earth System Models using existing model output from model intercomparison exercises. Finally, they explored the model processes that are driving simulated variability and trends.\r\n\r\nThe results inform the scientific community as to the fidelity of Earth System Models. This project helped to improve our models and give us more confidence in our predictions.\r\n\r\nThe overall objective of this project was to develop and implement a framework capable of evaluating the sensitivity of atmospheric composition simulated by ESMs to changing climate and emissions. \r\n\r\nOur scientific objectives were to:\r\n\r\nO1. Develop observationally-based metrics and relationships with which to evaluate variability and trends in atmospheric composition and its drivers in ESMs.   \r\n\r\nO2. Understand the sensitivity of observed and simulated atmospheric composition to environmental drivers.\r\n\r\nO3. Quantify the ability of ESMs to capture observed temporal variability and trends in atmospheric composition.\r\n\r\nO4. Improve our understanding of the processes driving observed variability in atmospheric composition."
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                    "abstract": "This dataset collection presents a global surface ozone compilation for long-term trends and ESM (Earth System Model) evaluation.\r\n\r\nThe project (Process Based Earth System Model Evaluation) brought together all publicly available surface ozone observations from online databases from the modern era to build a consistent dataset for the evaluation of chemical transport and chemistry-climate (Earth System) models for projects such as the Chemistry-Climate Model Initiative (CCMI) and Aer-Chem-MIP.  \r\n\r\nFrom a total dataset of approximately 6600 sites and 500 million hourly observations from 1971-2015, approximately 2200 sites and 200 million hourly observations pass screening as high-quality sites in regional background locations that are appropriate for use in global model evaluation. There was generally good data volume in the datasets since the start of air quality monitoring networks in 1990 through to 2013. Ozone observations are biased heavily toward North America and Europe with sparse coverage over the rest of the globe.  \r\n\r\nThis dataset collection was made available for the purposes of model evaluation as a set of gridded metrics intended to describe the distribution of ozone concentrations on monthly and annual timescales. This collection currently holds version 2.4 data only, but future versions may follow."
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            "title": "Vertical wind profile data from 6th November 2013 to 18th January 2016 measured by the University of Manchester 1290 mhz mobile wind profiler deployed on long term observations at Met Office Research Unit, Cardington, Bedfordshire",
            "abstract": "Vertical profiles of horizontal and vertical wind components as well as signal-to-noise (SNR) and spectal width measurements were collected at the Met Office Research Unit, Cardington, Bedfordshire, UK, from 6th November 2013 to 18th January 2016 as part of ongoing long term observations made by the NERC National Centre for Atmospheric Science (NCAS). These data were collected by the NCAS Atmospheric Measurement Facility's (AMF) 1290 MHz Mobile Wind Profiler, owned and operated by the University of Manchester and previously known as the aber-radar-1290mhz at the time of these observations. The data are available at 15 minute intervals as netCDF files to all registered BADC users under the Open Government License.\r\n\r\nPlease note, the data between 1st September and 31st December 2014 should be treated with caution as there were various logged errors during this period.\r\n\r\nThe dataset contains the following measurements:\r\n\r\nEastward wind velocity component\r\nNorthward wind velocity component\r\nUpward air velocity\r\nDirection the wind is from\r\nSignal to noise ratio\r\nAltitude of instrument above the ground\r\nLongitude of instrument\r\nLatitude of instrument\r\nSpectral width",
            "creationDate": "2022-07-22T09:15:57.183554",
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            "dataLineage": "Data were collected by the wind profiler before being processed by the instrument scientist, Emily Norton, and then provided to the BADC for archiving.",
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            "keywords": "NCAS, AMF, radar, wind profiler, boundary layer wind profiler, turbulence, thermals, boundary layer structure, radar wind profiler, Doppler radar, UHF radar, 'Clear' air radar, morning transition, convective boundary layer, mixed layer, entrainment zone, transitional boundary layer, nocturnal boundary layer, lower level jet, nocturnal jet, weather fronts, sting jets",
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                "title": "Acquisition Process for: Vertical wind profile data from 14th April 2010 to 25th May 2011 measured by the University of Manchester 1290 mhz mobile wind profiler deployed on long term observations at Met Office Research Unit, Cardington, Bedfordshire",
                "abstract": "This acquisition is comprised of the following: INSTRUMENTS: University of Manchester Degreane 1290mhz Mobile Wind Profiler Radar - formerly aber-radar-1290mhz; PLATFORMS: Met Office Meteorologial Research Unit, Cardington; "
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                    "abstract": "The Natural Environment Research Council's (NERC) National Centre for Atmospheric Science (NCAS) undertake a number of long term measurements by a suite of instruments to support ongoing atmospheric research at a variety of locations. These include a long-term observation mode of instruments from the NCAS Atmospheric Measurement Facility (AMF) when not deployed on specific field campaign duties for other projects. One such long-term deployment covers the NCAS mobile wind profiler deployed at the Met Office's Cardington site in Bedfordshire. This complements other long-term wind profilers in the UK, incuding the NERC Mesosphere-Stratosphere-Troposphere (MST) radar located near Absersystwyth, mid-Wales  - an alternative site also used for the NCAS AMF mobile wind profiler for long-term observations."
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                    "abstract": "The UK's Natural Environment Research Council's (NERC) National Centre for Atmospheric Sciences (NCAS) operates a suite of instrumentation to monitor the atmospheric dynamics and composition of the atmosphere. This dataset brings together all the long term routine observations made by NCAS instruments covering surface based instruments as well as remote sensing instruments such as radars and lidars. Some of the instruments may also be deployed elsewhere on field campaigns, for which the data will be available under the associated field campaign dataset. Links are also available to pages describing the instruments from which links to all data from that particular instrument can be found."
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                    "abstract": "Global Observatory of Lake Responses to Environmental Change (GloboLakes) was a project funded by the Natural Environment Research Council (NERC) with the following grant references; NE/J023345/2, NE/J02211X/1, NE/J023396/1, NE/J021717/1 and NE/J022810/1. These grants were led by Professor Christopher Merchant, Dr Mark Cutler, Mr Stephen Groom, Professor Stephen Maberly and Dr Claire Miller respectively. \r\n\r\nThere are around 304 million lakes globally. These provide essential resources for human survival and are an important component of global biogeochemical cycles. Lakes are also fragile systems that are sensitive to multiple pressures including nutrient enrichment, climate change and hydrological modification, making them important 'sentinels' of environmental perturbation. However, traditional monitoring has only produced data from a tiny fraction of the global population of lakes and disentangling the causes of change requires consistently-produced data from a large number of lakes, along with measurements of possible causes of change. Satellite observations (remote sensing) and the establishment of a global lake observatory would produce a step-change in our ability to detect and attribute the causes of changes in lakes world-wide. \r\n\r\nThis is now possible for three reasons: \r\n(1) the improved wavebands, spatial resolution and frequency of data collection from satellite sensors is now sufficient to monitor inland waters; \r\n(2) formulae to correct for atmospheric properties and to convert the detected reflected light to useful lake properties have been developed; and \r\n(3) computing power has increased to the point that allows near real time and archived information from satellites to be processed. \r\n\r\nGloboLakes analysed 20 years of data from more than 1000 large lakes across the globe to determine 'what controls the differential sensitivity of lakes to environmental perturbation'. \r\n\r\nThis was an ambitious project that was only possible by bringing together a consortium of scientists with complementary skills. These included expertise in remote sensing of freshwaters and processing large volumes of satellite images, collation and analysis of large-scale environmental data, environmental statistics and the assessment of data uncertainty, freshwater ecology and mechanisms of environmental change and the ability to produce lake models to forecast future lake conditions. \r\n\r\nThe eight objectives of GloboLakes were to:\r\n(i) develop remote sensing algorithms to estimate lake biogeochemical and physical parameters;\r\n(ii) make these algorithms operational and process satellite data;\r\n(iii) compile integrated spatio-temporal information on climatic and catchment data for >1000 lakes;\r\n(iv) integrate data and assess uncertainty in data sources;\r\n(v) detect spatial and temporal patterns in lake water quality;\r\n(vi) attribute the causes of lake response to environmental conditions;\r\n(vii) forecast lake sensitivity to environmental change;\r\n(viii) apply data to lake management and the monitoring of freshwater resources.\r\n\r\nThe project focused on the retrieval of surface water temperature as this has a fundamental effect on lake ecology, the concentration of coloured dissolved organic matter and suspended solids that derive largely from the catchment, the abundance of phytoplankton measured as the concentration of the pigment, chlorophyll a, and the abundance of cyanobacteria (blue-green algae) that can potentially be toxic. Knowledge of the conditions of lakes and their sensitivity to change is also extremely valuable for the management of lakes and reservoirs and GloboLakes provided information and products specifically for environmental managers. \r\n\r\nA satellite launched during the course of the project, called Sentinel 2, provided even greater spatial resolution allowing data to be collected and exploited from even smaller lakes. This was investigated by GloboLakes and incorporated into the framework of a global lake observatory."
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