Raw data acquired by position sensors on board RV Heincke during expedition HE662 were processed to receive a validated master track which can be used as reference of further expedition data. During HE662 the inertial navigation system IXSEA PHINS III and the GPS receivers Trimble Marine SPS461 and SAAB R5 SUPREME NAV were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.awi.de) with a resolution of 1 sec. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
Conductivity-temperature-depth profiles were measured using a CTD. The CTD was equipped with duplicate sensors for temperature, conductivity and oxygen. All sensors are calibrated irregularly.
Stäube sind feste Teilchen der Außenluft, die nicht sofort zu Boden sinken, sondern eine gewisse Zeit in der Atmosphäre verweilen. Nach ihrer Größe werden Staubpartikel in verschiedene Klassen eingeteilt. Als Feinstaub (PM10) bezeichnet man Partikel mit einem aerodynamischen Durchmesser von weniger als 10 Mikrometer (µm). Von diesen Partikeln besitzt ein Teil einen aerodynamischen Durchmesser, der kleiner ist als 2,5 µm (PM2,5). Hierzu gehört auch die Fraktion der ultrafeinen Partikel (< 0,1µm). Dargestellt wird der Durchschnitt aller Messwerte eines Sensors der letzten 5 Minuten Die dargestellten Messwerte wurden auf hohe und niedrige Ausreißer gefiltert. - Hohe Ausreißer sind alles jenseits des 3. Quartils + 1,5 * des Inter-Quartils-Bereichs (IQB) - Niedrige Ausreißer sind alles unterhalb des 1. Quartils - 1,5 * IQB
Die Messwerte wurden mittels des Sensor-Modells "Bosch BME280" erfasst.
Die Messwerte wurden mittels des Sensor-Modells "Bosch BME280" erfasst.
Die Messwerte wurden mittels des Sensor-Modells "Dallas semiconductor DS18B20" erfasst.
The AVHRR Mulitchannel Sea Surface Temperature Map (MCSST) was the first result of DLR's AVHRR pathfinder activities. The goal of the product is to provide the user with actual Sea Surface Temperature (SST) maps in a defined format easy to access with the highest possible reliability on the thematic quality. After a phase of definition, the operational production chain was launched in March 1993 covering the entire Mediterranean Sea and the Black Sea. Since then, daily, weekly, and monthly data sets have been available until September 13, 1994, when the AVHRR on board the NOAA-11 spacecraft failed. The production of daily, weekly and monthly SST maps was resumed in February, 1995, based on NOAA-14 AVHRR data. The NOAA-14 AVHRR sensor became some technical difficulties, so the generation was stopped on October 3, 2001. Since March 2002, NOAA-16 AVHRR SST maps are available again. With the beginning of January 2004, the data of AVHRR on board of NOAA-16 exhibited some anormal features showing strips in the scenes. Facing the “bar coded” images of NOAA16-AVHRR which occurred first in September 2003, continued in January 2004 for the second time and appeared in April 2004 again, DFD has decided to stop the reception of NOAA16 data on April 6th, 2004, and to start the reception of NOAA-17 data on this day. On April 7th, 2004, the production of all former NOAA16-AVHRR products as e.g. the SST composites was successully established. NOAA-17 is an AM sensor which passes central Europe about 2 hours earlier than NOAA-16 (about 10:00 UTC instead of 12:00 UTC for NOAA-16). In spring 2007, the communication system of NOAA-17 has degraded or is operating with limitations. Therefore, DFD has decided to shift the production of higher level products (NDVI, LST and SST) from NOAA-17 to NOAA-18 in April 2007. In order to test the performance of our processing chains, we processed simultaneously all NOAA-17 and NOAA-18 data from January 1st, 2007 till March 29th, 2007. All products are be available via EOWEB. Please remember that NOAA-18 is a PM sensor which passes central Europe about 1.5 hours later than NOAA-17 (about 11:30 UTC instead of 10:00 UTC for NOAA17). The SST product is intended for climate modelers, oceanographers, and all geo science-related disciplines dealing with ocean surface parameters. In addition, SST maps covering the North Atlantic, the Baltic Sea, the North Sea and the Western Atlantic equivalent to the Mediterranean MCSST maps are available since August 1994. The most important aspects of the MCSST maps are a) correct image registration and b) reasonable cloud screening to ensure that only cloud free pixels are taken for the later processing and compositing c) for deriving MCSST, only channel 4 and 5 are used.. The SST product consists of one 8 bit channel. For additional information, please see: https://wdc.dlr.de/sensors/avhrr/
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