dot
Detailansicht
Katalogkarte GBA
Katalogkarte ISBD
Suche präzisieren
Drucken
Download RIS
Hier klicken, um den Treffer aus der Auswahl zu entfernen
Titel Time of emergence of trends in ocean biogeochemistry
VerfasserIn Kathrin M. Keller, Fortunat Joos, Christoph C. Raible
Konferenz EGU General Assembly 2015
Medientyp Artikel
Sprache Englisch
Digitales Dokument PDF
Erschienen In: GRA - Volume 17 (2015)
Datensatznummer 250105236
Publikation (Nr.) Volltext-Dokument vorhandenEGU/EGU2015-4711.pdf
 
Zusammenfassung
The detection of forced trends in biogeochemical cycles and ecosystems is a challenge. A major issue is the presence of natural variability which has the potential to enhance or mask trends over decadal timescales. The successful detection of trend signals is thus a signal-to-noise (S/N) problem, i.e., the signal has to be of a magnitude that durably exceeds the envelope of background variability. One possible measure to estimate this is the time of emergence (ToE) of a signal, that is, the point in time at which the ratio S/N exceeds a certain threshold. We use historical simulations from 17 Earth System Models to investigate the ToE of trends in surface ocean biogeochemistry. For maximum comparability with the available observations, we focus on dissolved inorganic carbon (DIC), pCO2 and pH, and sea-surface temperature (SST). We find that signals in ocean biogeochemical variables emerge on much shorter timescales than the physical variable SST. The ToE patterns of pCO2 and pH are spatially very similar to DIC, yet the trends emerge much faster – after roughly 12 years for the majority of the global ocean area, compared to between 10-30 years for DIC and 45-90 years for SST. In general, the background noise is of higher importance in determining ToE than the strength of the trend signal. In areas with high natural variability, even strong trends both in the physical climate and carbon cycle system are masked by variability over decadal timescales. In contrast to the trend, natural variability is affected by the seasonal cycle. This has important implications for observations, since it implies that intra-annual variability could question the representativeness of irregularly seasonal sampled measurements for the entire year and, thus, the interpretation of observed trends.