Data usage in ARC MFC Sample Clauses

Data usage in ARC MFC and satellite TACs Arctic in situ data are collected by CMEMS INSTAC. Part of the collected data have been used in both TACs and MFCs. Based on the survey and CMEMS Product User Mannuals and QUID reports, a summary of the usage of in situ data is given in Table 3.3.3a for TACs and Table 3.3.3b for Arctic MFC, corresponding to each product. The CMEMS product list covers a wide range of parameters: sea level, water temperature, salinity, currents, sea ice variables, wave variables, dissolved oxygen, nutrients, pH, carbon related variables, chl-a, ammonium, primary production, phytoplankton and zooplankton etc. For TACs, in situ observations are used mainly for calibration/validation (cal/val) of Level 3 (L3) and Level 4 (L4) products. For some secondary products, e.g. ice drift, in situ observations can also be used for developing retrieving algorithms. Currently only Sea Level (SL) -, Sea Surface Temperature (SST)- and Ocean Sea Ice (OSI) TACs use Arctic in situ observations. No Arctic in situ data are used in OC/Wind/Wave TACs. Temperature, salinity and biogeochemical profiles: For the profile data, the amount of data assimilated for reanalysis is about 4000-5000 T/S profiles per year, mainly from Argo, ITP and R/Vs during the period 1993-2016. For validation purpose, 300 chl-a profiles from BioArgo floats, which are special Argo floats mounted with biochemical measurement devices, are used for model validation. SST from surface drifters: they provide near real time (NRT), high quality SST measurements which are used in CMEMS for validating NRT forecast. Surface currents: they are mainly calculated from drifting buoys (with drogue at 15m). There are HF radars in Northern Norway but these are better assimilated by downstream services. Their coverage is not worth the effort for a large area like the Arctic. The drifter-derived surface currents are now used in the validation of NRT forecasts. Current profiles: they are taken from NABOS (Nansen and Xxxxxxxx Basins Observational System) moorings from University of Alaska Fairbanks (Microwave Temperature Profilers - MMTP), IMR moorings in the Barents Sea Opening and Bering Strait moorings from Applied Physics Lab. in University of Washington (APL-UW). The data are used for validating physical reanalysis. Ice drift: they are taken from the IABP (International Arctic Buoy Program) drifting buoys and used for validating the ice drift acceleration and its seasonal cycle in the physical reanalysis Waves (Significant ...
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Related to Data usage in ARC MFC

  • Data Usage We may use Data for the following purposes (in each case to the extent permitted by law):

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  • Actions We May Take if You Engage in Any Restricted Activities If we believe that you’ve engaged in any of these activities, we may take a number of actions to protect PayPal, its customers and others at any time in our sole discretion. The actions we make take include, but are not limited to, the following: • Terminate this user agreement, limit your account, and/or close or suspend your account, immediately and without penalty to us; • Refuse to provide the PayPal services to you in the future; • At any time and without liability, suspend, limit or terminate your access to our websites, software, systems (including any networks and servers used to provide any of the PayPal services) operated by us or on our behalf, your PayPal account or any of the PayPal services, including limiting your ability to pay or send money with any of the payment methods linked to your PayPal account, restricting your ability to send money or make withdrawals; • Hold your money to the extent and for so long as reasonably needed to protect against the risk of liability. You acknowledge that, as a non-exhaustive guide: • PayPal’s risk of liability in respect of card-funded payments that you receive can last until the risk of a chargeback closing in favour of the payer/buyer (as determined by card scheme rules) has passed. This depends on certain factors, including, without limitation:

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