Global climate closely links with the Arctic Ocean ecosystem especially in the Barents Sea. The distributions and correlations among chlorophyll-a (CHL), sea ice concentration (ICE), wind speed (WIND), sea surface temperature (SST) and mixed layer depth (MLD) are studied within the region of Barents Sea (70°N-80°N, 30°E−40°E) over the period 2003–2013. CHL increased from north to south in general. Ice melted rapidly in the southern region (70°N-75°N) and had less impact than SST on phytoplankton blooming. Melting ice in northern region (75°N-80°N) contributed significant source on phytoplankton development. WIND had negative correlations with CHL in spring blooming season and had positive correlations during autumn.

Dimethylsulfide (DMS) concentration and sea-to-air DMS flux are simulated using a comprehensive biogeochemical model. The key model parameters are calibrated using a genetic algorithm under contemporary climate conditions. Environmental factors and DMS sea-air flux are compared for 1$\times$CO₂ and 4$\times$CO₂ climate conditions. By 4$\times$CO₂, SST increases more than doubles, DMS increases 27.5%. Mean annual DMS sea-to-air flux increases 323%. The increase of DMS flux under 4$\times$CO₂ conditions indicates that Arctic climate may be counteracting with the warming by 4$\times$CO₂.

全球气候与北冰洋生态系统紧密相连，尤其是在巴伦支海。研究了巴伦支海（70°N）地区的叶绿素a（CHL），海冰浓度（ICE），风速（WIND），海面温度（SST）和混合层深度（MLD）之间的分布和相关性。 2003-2013年期间为-80°N，30°E−40°E）。CHL通常从北到南增加。冰在南部地区（70°N-75°N）迅速融化，对浮游植物开花的影响小于SST。北部地区（75°N-80°N）的融冰是浮游植物发展的重要来源。WIND在春季开花季节与CHL呈负相关，而在秋季呈正相关。

使用全面的生物地球化学模型模拟了二甲基硫（DMS）浓度和海对空DMS通量。在现代气候条件下，使用遗传算法对关键模型参数进行了校准。比较环境因素和DMS海气通量1$\times$CO ₂和4$\times$CO ₂气候条件。乘4$\times$CO ₂，SST增加两倍以上，DMS增加27.5％。DMS的年平均海空通量增加了323％。DMS通量在4以下的增加$\times$CO ₂条件表明北极气候可能与4$\times$CO ₂。