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NOAA Climate Data Record (CDR) of Monthly Outgoing Longwave Radiation (OLR), Version 2.2-1. CLIMATE APPLICATIONS: Earth Radiation Budget Tropical dynamics (ENSO, MJO, tropical expansion) Precipitation Climate model verification Solar Energy Forecast

CLIMATE APPLICATIONS: global cloud climatologies climate research (monitoring and modelling), NMHSs & government agencies, private and public sector

CLIMATE APPLICATIONS: global cloud climatologies climate research (monitoring and modelling), NMHSs & government agencies, private and public sector

CLIMATE APPLICATIONS: PATMOS-x AVHRR supports: NCEI AVHRR Aerosol TCDR, Climate analysis, Climate model verification

CLARA-A1. CLIMATE APPLICATIONS: earth radiation budget studies climate research (monitoring and modelling), NMHSs & government agencies

CLIMATE APPLICATIONS: global cloud climatologies climate research (monitoring and modelling), NMHSs & government agencies, private and public sector

NOAA Climate Data Record (CDR) of AVHRR Daily and Monthly Aerosol Optical Thickness over Global Oceans, Version 2.0. CLIMATE APPLICATIONS: Aerosol climate forcing, climate model evaluation, long-term trend of air quality, etc.

CLIMATE APPLICATIONS: This CDR is used by an international community of scientists (https://www.ghrsst.org/ and others) to monitor the global ocean sea surface temperatures through the generation of level-4 climatology and daily optimally interpolated SST products, to give scientists valuable insights into ocean ecology by helping them to monitor coral reef stress, El Nino La Nina cycles that influence a wide range of weather conditions, to characterize local habitats, ocean current patterns and for college and high school training to study different oceanographic processes.

CLIMATE APPLICATIONS: PATMOS-x AVHRR supports 1. FCDR used by CM-SAF 2. FCDR and TCDR used for NCEI AVHRR Aerosol TCDR 3. Climate analysis 4. Climate model verification

ESA SST CCI Analysis L4 Long-term product (v1.1). CLIMATE APPLICATIONS: SST CCI records include the skin (radiometric) temperature at time of satellite observation and an estimate of SST at drifting buoy depth (20 cm) at a standardised time of day. The "calibration" of the retrieval is preserves independence from in situ observations. Context-specific uncertainty estimates are provided with each SST datum. In climate assessment activities, the SST CCI products have been found to be suitable for purposes such as evaluation of the mean state and (co)variability of coupled climate models. For further information see: http://www.esa-sst-cci.org/sites/default/files/Documents/public/SST_CCI-CAR-UKMO-001-Issue_1-signed-accepted.pdf.