Control of biological exposure to UV radiation in the Arctic Ocean: Comparison of the roles of ozone and riverine dissolved organic matter

Citation
Jae. Gibson et al., Control of biological exposure to UV radiation in the Arctic Ocean: Comparison of the roles of ozone and riverine dissolved organic matter, ARCTIC, 53(4), 2000, pp. 372-382
Citations number
52
Categorie Soggetti
Multidisciplinary
Journal title
ARCTIC
ISSN journal
00040843 → ACNP
Volume
53
Issue
4
Year of publication
2000
Pages
372 - 382
Database
ISI
SICI code
0004-0843(200012)53:4<372:COBETU>2.0.ZU;2-D
Abstract
Reports of severe stratospheric ozone depletion over the Arctic have height ened concern about the potential impact of rising ultraviolet-B (UV-B) radi ation on north polar aquatic ecosystems. Our optical measurements and model ling results indicate that the ozone-related UV-B influence on food web pro cesses in the Arctic Ocean is likely to be small relative to the effects ca used by variation in the concentrations of natural UV-absorbing compounds, known as chromophoric dissolved organic matter (CDOM), that enter the Arcti c basin via its large river inflows. The aim of our present study was to de velop and apply a simple bio-optical index that takes into account the comb ined effects of attenuation by atmospheric ozone and water column CDOM, and photobiological weighting for high-latitude environments such as the Arcti c Ocean. To this end, we computed values for a biologically effective UV do se rate parameter ("weighted transparency" or T*) based on underwater UV me asurements in high-latitude lakes and rivers that discharge into the Arctic Ocean; measured incident UV radiation at Barrow, Alaska: and published bio logical weighting curves for UV-induced DNA damage and UV photoinhibition o f photosynthesis. The results underscore how strongly the Arctic Ocean is i nfluenced by riverine inputs: shifts in CDOM loading (e.g., through climate change, land-use practices, or changes in ocean circulation) can cause var iations in biological UV exposure of much greater magnitude than ozone-rela ted effects.