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  • 1
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Phytoplankton size structure is acknowledged as a fundamental property determining energy flow through ‘microbial’ or ‘herbivore’ pathways. The balance between these two pathways determines the ability of the ecosystem to recycle carbon within the upper layer or to ...
    Type of Medium: Electronic Resource
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  • 2
    Publication Date: 2023-03-17
    Keywords: ATOS2; ATOS2/20-1; ATOS2/22-1; ATOS2/23-1; ATOS2/24-1; ATOS2/26-1; ATOS2/28-1; ATOS2/29-1; ATOS2/30-1; ATOS2/31-1; ATOS2/33-1; ATOS2/85-1; ATOS2/87-1; ATOS2/89-1; ATOS2/90-1; ATOS2/91-1; ATOS2/92-1; Calculated; Chlorophyll fluorescence raw data; CTD, Sea-Bird, SBE 911; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Hespérides; Latitude of event; Longitude of event; Oxygen; Pressure, water; Salinity; Scotia Sea, southwest Atlantic; Temperature, water; Temperature, water, potential; Transmission of light; Weddell Sea
    Type: Dataset
    Format: text/tab-separated-values, 58120 data points
    Location Call Number Expected Availability
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  • 3
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Hellmer, Hartmut H; Huhn, Oliver; Gomis, Damià; Timmermann, Ralph (2011): On the freshening of the northwestern Weddell Sea continental shelf. Ocean Science, 7(3), 305-316, https://doi.org/10.5194/os-7-305-2011
    Publication Date: 2023-10-28
    Description: We analyzed hydrographic data from the northwestern Weddell Sea continental shelf of the three austral winters 1989, 1997, and 2006 and two summers following the last winter cruise. During summer a thermal front exists at ~64° S separating cold southern waters from warm northern waters that have similar characteristics as the deep waters of the central basin of the Bransfield Strait. In winter, the whole continental shelf exhibits southern characteristics with high Neon (Ne) concentrations, indicating a significant input of glacial melt water. The comparison of the winter data from the shallow shelf off the tip of the Antarctic Peninsula, spanning a period of 17 yr, shows a salinity decrease of 0.09 for the whole water column, which has a residence time of 〈1 yr. We interpret this freshening as being caused by a combination of reduced salt input due to a southward sea ice retreat and higher precipitation during the late 20th century on the western Weddell Sea continental shelf. However, less salinification might also result from a delicate interplay between enhanced salt input due to sea ice formation in coastal areas formerly occupied by Larsen A and B ice shelves and increased Larsen C ice loss.
    Keywords: 06AQANTIX_2/100-1; 06AQANTIX_2/101-1; 06AQANTIX_2/102-1; 06AQANTIX_2/103-1; 06AQANTIX_2/104-1; 06AQANTIX_2/105-1; 06AQANTIX_2/106-1; 06AQANTIX_2/108-1; 06AQANTIX_2/108-2; 06AQANTIX_2/109-1; 06AQANTIX_2/113-1; 06AQANTIX_2/114-2; 06AQANTIX_2/115-1; 06AQANTIX_2/115-2; 06AQANTIX_2/35-1; 06AQANTIX_2/36-1; 06AQANTIX_2/39-1; 06AQANTIX_2/40-1; 06AQANTIX_2/41-1; 06AQANTIX_2/42-1; 06AQANTIX_2/43-1; 06AQANTIX_2/44-1; 06AQANTIX_2/45-1; 06AQANTIX_2/45-2; 06AQANTIX_2/46-1; 06AQANTIX_2/47-1; 06AQANTIX_2/48-1; 06AQANTIX_2/48-2; 06AQANTIX_2/49-1; 06AQANTIX_2/50-1; 06AQANTIX_2/51-1; 06AQANTIX_2/53-1; 06AQANTIX_2/55-1; 06AQANTIX_2/56-1; 06AQANTIX_2/56-2; 06AQANTIX_2/57-1; 06AQANTIX_2/58-1; 06AQANTIX_2/59-1; 06AQANTIX_2/60-1; 06AQANTIX_2/61-1; 06AQANTIX_2/62-1; 06AQANTIX_2/63-1; 06AQANTIX_2/63-2; 06AQANTIX_2/64-1; 06AQANTIX_2/65-1; 06AQANTIX_2/66-1; 06AQANTIX_2/67-1; 06AQANTIX_2/68-1; 06AQANTIX_2/69-1; 06AQANTIX_2/70-1; 06AQANTIX_2/71-1; 06AQANTIX_2/72-1; 06AQANTIX_2/73-1; 06AQANTIX_2/74-1; 06AQANTIX_2/75-1; 06AQANTIX_2/75-2; 06AQANTIX_2/76-1; 06AQANTIX_2/77-1; 06AQANTIX_2/78-1; 06AQANTIX_2/79-1; 06AQANTIX_2/80-1; 06AQANTIX_2/81-1; 06AQANTIX_2/82-1; 06AQANTIX_2/83-1; 06AQANTIX_2/84-1; 06AQANTIX_2/85-1; 06AQANTIX_2/86-1; 06AQANTIX_2/87-1; 06AQANTIX_2/88-1; 06AQANTIX_2/89-1; 06AQANTIX_2/90-1; 06AQANTIX_2/91-1; 06AQANTIX_2/92-1; 06AQANTIX_2/93-1; 06AQANTIX_2/94-1; 06AQANTIX_2/94-2; 06AQANTIX_2/95-1; 06AQANTIX_2/96-1; 06AQANTIX_2/97-1; 06AQANTIX_2/98-1; 06AQANTIX_2/99-1; 06AQANTVIII_2/119-1; 06AQANTVIII_2/124-1; 06AQANTVIII_2/129-1; 06AQANTVIII_2/134-1; 06AQANTVIII_2/137-1; 06AQANTVIII_2/138-1; 06AQANTVIII_2/139-1; 06AQANTVIII_2/141-1; 06AQANTVIII_2/142-1; 06AQANTVIII_2/144-1; 06AQANTVIII_2/145-1; 06AQANTVIII_2/146-1; 06AQANTVIII_2/147-1; 06AQANTVIII_2/148-1; 06AQANTVIII_2/149-1; 06AQANTVIII_2/150-1; 06AQANTVIII_2/151-1; 06AQANTVIII_2/152-1; 06AQANTVIII_2/153-1; 06AQANTVIII_2/154-1; 06AQANTVIII_2/155-1; 06AQANTVIII_2/156-1; 06AQANTVIII_2/157-1; 06AQANTVIII_2/158-2; 06AQANTVIII_2/159-1; 06AQANTVIII_2/160-1; 06AQANTVIII_2/161-1; 06AQANTVIII_2/162-1; 06AQANTVIII_2/163-1; 06AQANTVIII_2/164-1; 06AQANTVIII_2/165-1; 06AQANTVIII_2/166-1; 06AQANTVIII_2/167-1; 06AQANTVIII_2/168-1; 06AQANTVIII_2/169-1; 06AQANTVIII_2/170-1; 06AQANTVIII_2/171-1; 06AQANTVIII_2/172-1; 06AQANTVIII_2/173-1; 06AQANTVIII_2/174-1; 06AQANTVIII_2/175-1; 06AQANTVIII_2/176-1; 06AQANTVIII_2/177-1; 06AQANTVIII_2/178-1; 06AQANTVIII_2/179-1; 06AQANTVIII_2/180-1; 06AQANTVIII_2/181-1; 06AQANTVIII_2/182-1; 06AQANTVIII_2/183-1; 06AQANTVIII_2/184-1; 06AQANTVIII_2/185-1; 06AQANTVIII_2/186-1; 06AQANTVIII_2/187-1; 06AQANTVIII_2/188-1; 06AQANTVIII_2/189-1; 06AQANTVIII_2/192-1; 06AQANTVIII_2/193-1; 06AQANTVIII_2/194-1; 06AQANTVIII_2/195-1; 06AQANTVIII_2/197-1; 06AQANTVIII_2/198-1; 06AQANTVIII_2/199-1; 06AQANTVIII_2/200-1; 06AQANTVIII_2/201-1; 06AQANTVIII_2/202-1; 06AQANTVIII_2/203-1; 06AQANTVIII_2/204-1; 06AQANTVIII_2/205-1; 06AQANTVIII_2/206-1; 06AQANTVIII_2/207-1; 06AQANTVIII_2/208-1; 06AQANTVIII_2/209-1; 06AQANTVIII_2/210-1; 06AQANTVIII_2/211-1; 06AQANTVIII_2/212-1; 06AQANTVIII_2/213-1; 06AQANTVIII_2/214-1; 06AQANTVIII_2/215-1; 06AQANTVIII_2/216-1; 06AQANTVIII_2/217-1; 06AQANTVIII_2/218-1; 06AQANTVIII_2/219-1; 06AQANTVIII_2/220-1; 06AQANTVIII_2/221-1; 06AQANTVIII_2/222-1; 06AQANTVIII_2/223-1; 06AQANTXIII_4/100-1; 06AQANTXIII_4/10-1; 06AQANTXIII_4/101-1; 06AQANTXIII_4/102-2; 06AQANTXIII_4/103-1; 06AQANTXIII_4/11-1; 06AQANTXIII_4/12-1; 06AQANTXIII_4/13-1; 06AQANTXIII_4/13-3; 06AQANTXIII_4/14-3; 06AQANTXIII_4/15-2; 06AQANTXIII_4/15-4; 06AQANTXIII_4/16-1; 06AQANTXIII_4/17-1; 06AQANTXIII_4/18-1; 06AQANTXIII_4/19-1; 06AQANTXIII_4/19-3; 06AQANTXIII_4/20-1; 06AQANTXIII_4/2-1; 06AQANTXIII_4/21-1; 06AQANTXIII_4/2-2; 06AQANTXIII_4/22-1; 06AQANTXIII_4/22-3; 06AQANTXIII_4/23-1; 06AQANTXIII_4/24-1; 06AQANTXIII_4/25-1; 06AQANTXIII_4/25-3; 06AQANTXIII_4/26-1; 06AQANTXIII_4/27-1; 06AQANTXIII_4/28-1; 06AQANTXIII_4/28-3; 06AQANTXIII_4/29-1; 06AQANTXIII_4/30-1; 06AQANTXIII_4/3-1; 06AQANTXIII_4/31-1; 06AQANTXIII_4/31-4; 06AQANTXIII_4/32-1; 06AQANTXIII_4/33-1; 06AQANTXIII_4/34-1; 06AQANTXIII_4/34-3; 06AQANTXIII_4/34-4; 06AQANTXIII_4/35-1; 06AQANTXIII_4/35-4; 06AQANTXIII_4/36-1; 06AQANTXIII_4/37-1; 06AQANTXIII_4/38-1; 06AQANTXIII_4/38-4; 06AQANTXIII_4/39-1; 06AQANTXIII_4/40-1; 06AQANTXIII_4/4-1; 06AQANTXIII_4/41-1; 06AQANTXIII_4/42-1; 06AQANTXIII_4/43-1; 06AQANTXIII_4/44-1; 06AQANTXIII_4/44-3; 06AQANTXIII_4/45-1; 06AQANTXIII_4/46-1; 06AQANTXIII_4/47-1; 06AQANTXIII_4/48-1; 06AQANTXIII_4/48-3; 06AQANTXIII_4/49-1; 06AQANTXIII_4/50-1; 06AQANTXIII_4/5-1; 06AQANTXIII_4/51-1; 06AQANTXIII_4/52-1; 06AQANTXIII_4/52-3; 06AQANTXIII_4/5-3; 06AQANTXIII_4/53-1; 06AQANTXIII_4/54-1; 06AQANTXIII_4/54-3; 06AQANTXIII_4/55-1; 06AQANTXIII_4/56-2; 06AQANTXIII_4/56-4; 06AQANTXIII_4/57-1; 06AQANTXIII_4/57-4; 06AQANTXIII_4/58-1; 06AQANTXIII_4/59-1; 06AQANTXIII_4/60-1; 06AQANTXIII_4/60-4; 06AQANTXIII_4/6-1; 06AQANTXIII_4/61-1; 06AQANTXIII_4/62-1; 06AQANTXIII_4/62-3; 06AQANTXIII_4/63-1; 06AQANTXIII_4/65-2; 06AQANTXIII_4/66-1; 06AQANTXIII_4/66-3; 06AQANTXIII_4/67-1; 06AQANTXIII_4/68-1; 06AQANTXIII_4/69-1; 06AQANTXIII_4/70-1; 06AQANTXIII_4/7-1; 06AQANTXIII_4/71-1; 06AQANTXIII_4/71-5; 06AQANTXIII_4/7-2; 06AQANTXIII_4/72-1; 06AQANTXIII_4/73-1; 06AQANTXIII_4/74-2; 06AQANTXIII_4/75-1; 06AQANTXIII_4/75-4; 06AQANTXIII_4/76-1; 06AQANTXIII_4/77-1; 06AQANTXIII_4/78-1; 06AQANTXIII_4/79-1; 06AQANTXIII_4/79-3; 06AQANTXIII_4/80-1; 06AQANTXIII_4/8-1; 06AQANTXIII_4/81-1; 06AQANTXIII_4/82-1; 06AQANTXIII_4/83-1; 06AQANTXIII_4/83-2; 06AQANTXIII_4/84-1; 06AQANTXIII_4/85-1; 06AQANTXIII_4/86-1; 06AQANTXIII_4/86-3; 06AQANTXIII_4/87-1; 06AQANTXIII_4/88-1; 06AQANTXIII_4/89-1; 06AQANTXIII_4/90-1; 06AQANTXIII_4/90-4; 06AQANTXIII_4/9-1; 06AQANTXIII_4/91-1; 06AQANTXIII_4/92-1; 06AQANTXIII_4/93-1; 06AQANTXIII_4/94-1; 06AQANTXIII_4/94-3; 06AQANTXIII_4/95-1; 06AQANTXIII_4/96-1; 06AQANTXIII_4/97-1; 06AQANTXIII_4/98-1; 06AQANTXIII_4/99-1; 06AQANTXIII_4/99-4; 06AQANTXV_4/100-1; 06AQANTXV_4/10-1; 06AQANTXV_4/101-1; 06AQANTXV_4/102-1; 06AQANTXV_4/103-1; 06AQANTXV_4/104-1; 06AQANTXV_4/105-1; 06AQANTXV_4/106-1; 06AQANTXV_4/107-2; 06AQANTXV_4/107-4; 06AQANTXV_4/108-1; 06AQANTXV_4/109-1; 06AQANTXV_4/1-1; 06AQANTXV_4/110-1; 06AQANTXV_4/111-1; 06AQANTXV_4/11-2; 06AQANTXV_4/112-1; 06AQANTXV_4/11-3; 06AQANTXV_4/113-1; 06AQANTXV_4/11-4; 06AQANTXV_4/114-2; 06AQANTXV_4/114-4; 06AQANTXV_4/11-5; 06AQANTXV_4/115-1; 06AQANTXV_4/11-6; 06AQANTXV_4/116-1; 06AQANTXV_4/117-1; 06AQANTXV_4/118-1; 06AQANTXV_4/119-1; 06AQANTXV_4/120-1; 06AQANTXV_4/12-1; 06AQANTXV_4/121-1; 06AQANTXV_4/122-1; 06AQANTXV_4/122-2; 06AQANTXV_4/123-1; 06AQANTXV_4/124-1; 06AQANTXV_4/125-1; 06AQANTXV_4/126-1; 06AQANTXV_4/127-1; 06AQANTXV_4/128-1; 06AQANTXV_4/129-1; 06AQANTXV_4/130-1; 06AQANTXV_4/13-1; 06AQANTXV_4/131-1; 06AQANTXV_4/132-1; 06AQANTXV_4/133-1; 06AQANTXV_4/134-1; 06AQANTXV_4/135-1; 06AQANTXV_4/136-1; 06AQANTXV_4/14-1; 06AQANTXV_4/15-1; 06AQANTXV_4/15-2; 06AQANTXV_4/16-1; 06AQANTXV_4/17-1; 06AQANTXV_4/18-1; 06AQANTXV_4/19-1; 06AQANTXV_4/20-1; 06AQANTXV_4/20-2; 06AQANTXV_4/2-1; 06AQANTXV_4/21-1; 06AQANTXV_4/22-1; 06AQANTXV_4/23-1; 06AQANTXV_4/24-1; 06AQANTXV_4/25-1; 06AQANTXV_4/26-1; 06AQANTXV_4/27-1; 06AQANTXV_4/28-1; 06AQANTXV_4/29-1; 06AQANTXV_4/30-1; 06AQANTXV_4/30-2; 06AQANTXV_4/31-1; 06AQANTXV_4/3-2; 06AQANTXV_4/32-1; 06AQANTXV_4/33-1; 06AQANTXV_4/34-1; 06AQANTXV_4/35-1; 06AQANTXV_4/36-1; 06AQANTXV_4/37-1; 06AQANTXV_4/38-1; 06AQANTXV_4/39-1; 06AQANTXV_4/40-1; 06AQANTXV_4/41-1; 06AQANTXV_4/42-1; 06AQANTXV_4/4-3; 06AQANTXV_4/43-1; 06AQANTXV_4/44-1; 06AQANTXV_4/45-1; 06AQANTXV_4/46-1; 06AQANTXV_4/47-1; 06AQANTXV_4/47-2; 06AQANTXV_4/48-1; 06AQANTXV_4/49-1; 06AQANTXV_4/50-1; 06AQANTXV_4/5-1; 06AQANTXV_4/51-1; 06AQANTXV_4/52-1; 06AQANTXV_4/53-1; 06AQANTXV_4/54-1; 06AQANTXV_4/55-1; 06AQANTXV_4/56-1; 06AQANTXV_4/57-1; 06AQANTXV_4/58-1; 06AQANTXV_4/59-1; 06AQANTXV_4/60-1; 06AQANTXV_4/6-1; 06AQANTXV_4/61-1; 06AQANTXV_4/62-1; 06AQANTXV_4/63-1; 06AQANTXV_4/65-1; 06AQANTXV_4/66-1; 06AQANTXV_4/67-1; 06AQANTXV_4/68-1; 06AQANTXV_4/68-2; 06AQANTXV_4/69-1;
    Type: Dataset
    Format: application/zip, 8 datasets
    Location Call Number Expected Availability
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  • 4
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: García, Marc A; Castro, Carmen G; Ríos, Aida F; Doval, María Dolores; Rosón, G; Gomis, Damià; López, Oriol (2002): Water masses and distribution of physico-chemical properties in the western Bransfield Strait and Gerlache Strait during Austral summer 1995/96. Deep Sea Research Part II: Topical Studies in Oceanography, 49(4-5), 585-602, https://doi.org/10.1016/S0967-0645(01)00113-8
    Publication Date: 2024-02-01
    Description: n the framework of the FRUELA project, two oceanographic surveys were conducted by R/V Hespérides in the eastern Bellingshausen Sea, western basin of the Bransfield Strait and Gerlache Strait area during December 1995 and January 1996. The main hydrographic structures of the study domain were the Southern Boundary of the ACC and the Bransfield Front. The characteristics and zonation of local water masses are discussed in terms of temperature, salinity, dissolved oxygen, nutrient and inorganic carbon concentrations. Concentration intervals for water mass labelling, on the basis of chemical parameters in addition to the common theta/S-based classification, are defined. Silicate seems to be a very good discriminator for local water masses.
    Keywords: JGOFS; Joint Global Ocean Flux Study
    Type: Dataset
    Format: application/zip, 2 datasets
    Location Call Number Expected Availability
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  • 5
    Publication Date: 2024-02-01
    Keywords: CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Fluorescence, chlorophyll; Fruela96; Fruela96_185; Fruela96_186; Fruela96_187; Fruela96_187.2; Fruela96_188; Fruela96_189; Fruela96_190; Fruela96_191; Fruela96_192; Fruela96_193; Fruela96_194; Fruela96_195; Fruela96_195.2; Fruela96_196; Fruela96_197; Fruela96_198; Fruela96_199; Fruela96_200; Fruela96_201; Fruela96_201.2; Fruela96_202; Fruela96_203; Fruela96_204; Fruela96_205; Fruela96_206; Fruela96_207; Fruela96_208; Fruela96_209; Fruela96_210; Fruela96_211; Fruela96_212; Fruela96_213; Fruela96_214; Fruela96_215; Fruela96_216; Fruela96_217; Fruela96_218; Fruela96_219; Fruela96_220; Fruela96_221; Fruela96_222; Fruela96_223; Fruela96_223.1; Fruela96_223.2; Fruela96_223.3; Fruela96_223.4; Fruela96_224; Fruela96_224.1; Fruela96_224.2; Fruela96_224.3; Fruela96_224.4; Fruela96_224.5; Fruela96_225.1; Fruela96_225.2; Fruela96_225.3; Fruela96_225.4; Fruela96_225.5; Fruela96_226; Fruela96_226.1; Fruela96_226.2; Fruela96_226.3; Fruela96_226.4; Fruela96_226.5; Fruela96_226.6; Fruela96_227.1; Fruela96_227.2; Fruela96_227.3; Fruela96_227.4; Fruela96_227.5; he31_234; he31_235; he31_236; he31_237; he31_238; he31_239; he31_240; he31_241; he31_242; he31_243; he31_244; he31_245; he31_246; he31_247; he31_248; he31_249; he31_250; he31_251; he31_252; he31_253; he31_254; he31_255; he31_256; he31_257; he31_258; he31_259; he31_260; he31_261; he31_262; he31_263; he31_264; he31_265; he31_266; he31_267; he31_268; he31_269; he31_270; he31_271; he31_272; he31_273; he31_274; he31_275; he31_276; he31_277; he31_278; he31_279; he31_280; he31_281; he31_282; he31_283; he31_284; he31_285; he31_286; he31_287; he31_288; he31_289; he31_290; he31_291; he31_292; he31_293; he31_294; he31_295; he31_296; he31_297; he31_298; he31_299; he31_300; he31_301; he31_302; Hespérides; JGOFS; Joint Global Ocean Flux Study; Latitude of event; Longitude of event; Number of observations; Pressure, water; Salinity; Temperature, water; Transmission of light
    Type: Dataset
    Format: text/tab-separated-values, 434637 data points
    Location Call Number Expected Availability
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  • 6
    Publication Date: 2024-02-01
    Keywords: Bransfield Strait; CTD; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Elevation of event; Event label; Fluorescence, chlorophyll; Fruela95; Fruela95_1; Fruela95_10; Fruela95_100; Fruela95_101; Fruela95_102; Fruela95_103; Fruela95_103.1; Fruela95_104; Fruela95_105; Fruela95_106; Fruela95_107; Fruela95_108; Fruela95_109; Fruela95_11; Fruela95_110; Fruela95_111; Fruela95_112; Fruela95_113; Fruela95_114; Fruela95_115; Fruela95_116; Fruela95_117; Fruela95_118; Fruela95_119; Fruela95_12; Fruela95_120; Fruela95_121; Fruela95_121.2; Fruela95_122; Fruela95_123; Fruela95_124; Fruela95_125; Fruela95_126; Fruela95_127; Fruela95_128; Fruela95_129; Fruela95_13; Fruela95_130; Fruela95_131; Fruela95_132; Fruela95_133; Fruela95_134; Fruela95_135; Fruela95_137; Fruela95_138; Fruela95_138.1; Fruela95_139; Fruela95_14; Fruela95_140; Fruela95_141; Fruela95_142; Fruela95_143; Fruela95_144; Fruela95_145; Fruela95_146; Fruela95_147; Fruela95_148; Fruela95_149; Fruela95_15; Fruela95_150; Fruela95_151; Fruela95_152; Fruela95_153; Fruela95_154; Fruela95_155; Fruela95_156; Fruela95_156.1; Fruela95_156.2; Fruela95_156.3; Fruela95_156.4; Fruela95_156.5; Fruela95_156.6; Fruela95_156.7; Fruela95_156.8; Fruela95_156.9; Fruela95_157; Fruela95_158; Fruela95_159; Fruela95_16; Fruela95_160; Fruela95_161; Fruela95_162; Fruela95_163; Fruela95_164; Fruela95_165; Fruela95_166; Fruela95_167; Fruela95_168; Fruela95_168.1; Fruela95_168.2; Fruela95_168.3; Fruela95_168.4; Fruela95_168.5; Fruela95_169; Fruela95_169.1; Fruela95_169.2; Fruela95_169.3; Fruela95_169.4; Fruela95_169.5; Fruela95_17; Fruela95_170; Fruela95_171; Fruela95_172; Fruela95_173; Fruela95_174; Fruela95_175; Fruela95_176; Fruela95_177; Fruela95_177.1; Fruela95_177.2; Fruela95_177.3; Fruela95_177.4; Fruela95_177.5; Fruela95_178; Fruela95_178.1; Fruela95_178.2; Fruela95_178.3; Fruela95_178.4; Fruela95_178.5; Fruela95_179; Fruela95_18; Fruela95_180; Fruela95_181; Fruela95_182; Fruela95_183; Fruela95_184; Fruela95_184.1; Fruela95_184.2; Fruela95_184.3; Fruela95_184.4; Fruela95_184.4a; Fruela95_184.5; Fruela95_19; Fruela95_2; Fruela95_20; Fruela95_21; Fruela95_22; Fruela95_23; Fruela95_24; Fruela95_25; Fruela95_26; Fruela95_27; Fruela95_28; Fruela95_29; Fruela95_3; Fruela95_30; Fruela95_31; Fruela95_32; Fruela95_33; Fruela95_34; Fruela95_34.1; Fruela95_35; Fruela95_36; Fruela95_36/37; Fruela95_36.1; Fruela95_37.1; Fruela95_38; Fruela95_38.1; Fruela95_39; Fruela95_39.1; Fruela95_4; Fruela95_40; Fruela95_41; Fruela95_42; Fruela95_44; Fruela95_45; Fruela95_45.3; Fruela95_46; Fruela95_47; Fruela95_47.1; Fruela95_48; Fruela95_49; Fruela95_49.1; Fruela95_5; Fruela95_50; Fruela95_51; Fruela95_52; Fruela95_52.1; Fruela95_53; Fruela95_54; Fruela95_55; Fruela95_56; Fruela95_57; Fruela95_58; Fruela95_59; Fruela95_6; Fruela95_60; Fruela95_61; Fruela95_62; Fruela95_63; Fruela95_64; Fruela95_65; Fruela95_66; Fruela95_67; Fruela95_68; Fruela95_69; Fruela95_7; Fruela95_70; Fruela95_71; Fruela95_72; Fruela95_73; Fruela95_74; Fruela95_74.1; Fruela95_75; Fruela95_76; Fruela95_77; Fruela95_78; Fruela95_78.1; Fruela95_79; Fruela95_8; Fruela95_80; Fruela95_81; Fruela95_82; Fruela95_83; Fruela95_84; Fruela95_85; Fruela95_86; Fruela95_87; Fruela95_88; Fruela95_89; Fruela95_9; Fruela95_90; Fruela95_91; Fruela95_92; Fruela95_93; Fruela95_94; Fruela95_95; Fruela95_96; Fruela95_97; Fruela95_98; Fruela95_99; Fruela95_99.1; he31_001; he31_002; he31_003; he31_004; he31_005; he31_006; he31_007; he31_008; he31_009; he31_010; he31_011; he31_012; he31_013; he31_014; he31_015; he31_016; he31_017; he31_018; he31_019; he31_020; he31_021; he31_022; he31_023; he31_024; he31_025; he31_026; he31_027; he31_028; he31_029; he31_030; he31_031; he31_032; he31_033; he31_034; he31_035; he31_036; he31_037; he31_039; he31_040; he31_041; he31_042; he31_043; he31_044; he31_045; he31_046; he31_047; he31_048; he31_049; he31_050; he31_051; he31_052; he31_053; he31_054; he31_055; he31_056; he31_057; he31_058; he31_059; he31_060; he31_061; he31_062; he31_063; he31_064; he31_065; he31_066; he31_067; he31_068; he31_069; he31_070; he31_071; he31_072; he31_073; he31_074; he31_075; he31_076; he31_077; he31_078; he31_079; he31_080; he31_081; he31_082; he31_083; he31_084; he31_085; he31_086; he31_087; he31_088; he31_089; he31_090; he31_091; he31_092; he31_093; he31_094; he31_095; he31_096; he31_097; he31_098; he31_099; he31_100; he31_101; he31_102; he31_103; he31_104; he31_105; he31_106; he31_107; he31_108; he31_109; he31_110; he31_111; he31_112; he31_113; he31_114; he31_115; he31_116; he31_117; he31_118; he31_119; he31_120; he31_121; he31_122; he31_123; he31_124; he31_125; he31_126; he31_127; he31_128; he31_129; he31_130; he31_131; he31_132; he31_133; he31_134; he31_135; he31_136; he31_137; he31_138; he31_139; he31_140; he31_141; he31_142; he31_143; he31_144; he31_145; he31_146; he31_147; he31_148; he31_149; he31_150; he31_151; he31_152; he31_153; he31_154; he31_155; he31_156; he31_157; he31_158; he31_159; he31_160; he31_161; he31_162; he31_163; he31_164; he31_165; he31_166; he31_167; he31_168; he31_169; he31_170; he31_171; he31_172; he31_173; he31_174; he31_175; he31_176; he31_177; he31_178; he31_179; he31_180; he31_181; he31_182; he31_183; he31_184; he31_185; he31_186; he31_187; he31_188; he31_189; he31_190; he31_191; he31_192; he31_193; he31_194; he31_195; he31_196; he31_197; he31_198; he31_199; he31_200; he31_201; he31_202; he31_203; he31_204; he31_205; he31_206; he31_207; he31_208; he31_209; he31_210; he31_211; he31_212; he31_213; he31_214; he31_215; he31_216; he31_217; he31_218; he31_219; he31_220; he31_221; he31_222; he31_223; he31_224; he31_225; he31_226; he31_227; he31_228; he31_229; he31_230; he31_231; he31_232; he31_233; Hespérides; JGOFS; Joint Global Ocean Flux Study; Latitude of event; Longitude of event; Number of observations; Pressure, water; Salinity; Temperature, water; Temperature, water, potential; Transmission of light
    Type: Dataset
    Format: text/tab-separated-values, 1150626 data points
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  • 7
    Publication Date: 2024-04-20
    Description: A coastal sea level reconstruction based on tide gauge observations is developed and applied to the western basin of the Mediterranean sea, including sea level anomaly (SLA) and interpolation error along the entire coastline. The reconstructions are carried out in four frequency bands: periods longer than 10 years, periods between 1 and 10 years, periods between 1 month and 1 year, and periods between 1day and 1month. Total sea level at monthly and daily resolution, obtained by merging the different frequency bands, is also provided. The reconstructions are based on an optimal interpolation method in which the correlation between tide gauge data and all coastal points has been determined from the outputs of the numerical model managed by the Balearic Islands Coastal Observing and Forecasting System (SOCIB, https://www.socib.es). The reconstructions for frequencies lower than 1 month use monthly observations from the Permanent Service for Mean Sea Level (PSMSL, https://www.psmsl.org/) database and cover the period from 1884 to 2019. For the reconstruction of higher frequencies, hourly observations from the Global Extreme Sea Level Analysis (GESLA–2, https://www.gesla.org/) dataset are used, and cover from 1980 to 2015.
    Keywords: Coastal sea level; Mediterranean Sea; Optimal interpolation; reconstruction; Tide gauge
    Type: Dataset
    Format: application/x-rar-compressed, 699.8 MBytes
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  • 8
    Publication Date: 2012-09-12
    Description: The hindcasts of residual sea surface are very useful tools for the design of infrastructures and coastal management applications, as well as for scientific studies on sea-level variability. In this paper we present VANI2-ERA, a new hindcast of residual sea surface covering the Mediterranean Sea and a sector of the NE Atlantic Ocean with a spatial resolution of 1/6°×1/4°. VANI2-ERA was obtained with a barotropic version of the HAMSOM model forced with a dynamical downscaling of the ERA40 reanalysis spanning the period 1958-2008. This new hindcast represents an update of the well-known HIPOCAS hindcast, which has been the reference dataset for the last few years. VANI2-ERA has been extensively validated with tide gauge observations distributed all around Southern Europe and compared with four other hindcasts, including HIPOCAS. The new hindcast shows smaller root mean square errors, higher correlation and higher variance reduction than any previous hindcasts at most stations. However, its performance is poorer than HIPOCAS in reproducing the magnitude of extreme events. Residual sea surface trends were also obtained and their uncertainty was assessed by means of a comparison between VANI2-ERA and HIPOCAS for the common period 1958-2001. Differences of up to 0.4±0.1 mm yr –1 between the two datasets are derived from the differences between the ERA40 and NCEP atmospheric reanalyses. The VANI2-ERA hindcast was also used to compare the variability of the period 1998-2008 with past decades, obtaining that the standard deviation of sea-level residuals has been 5-10% lower than for the period 1958-2008. The period 1998-2008 also shows a 20% reduction in the magnitude of positive extreme events, while negative extreme events have not changed significantly with respect to past decades. Finally, the trends computed for the period 1998-2008 are slightly positive (+0.11±0.04 mm yr –1 ) compared with the clearly negative trends obtained for the period 1958-2008.
    Print ISSN: 0214-8358
    Electronic ISSN: 1886-8134
    Topics: Agriculture, Forestry, Horticulture, Fishery, Domestic Science, Nutrition
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  • 9
    Publication Date: 1995-01-01
    Print ISSN: 0079-6611
    Electronic ISSN: 1873-4472
    Topics: Geosciences , Physics
    Published by Elsevier
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  • 10
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