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| 1 | The relationships among aerosol optical depth, ice, phytoplankton and dimethylsulfide and the implication for future climate in the Greenland Sea显示文摘The sea-to-air flux of dimethylsulphide(DMS) is one of the major sources of marine biogenic aerosol, and can have an important radiative impact on climate, especially in the Arctic Ocean. Satellite-derived aerosol optical depth(AOD) is used as a proxy for aerosol burden which is dominated by biogenic aerosol during summer and autumn. The spring sea ice melt period is a strong source of aerosol precursors in the Arctic. However, high aerosol levels in early spring are likely related to advection of continental pollution from the south(Arctic haze).Higher AOD was generally registered in the southern part of the study region. Sea ice concentration(SIC) and AOD were positively correlated, while cloud cover(CLD) and AOD were negative correlation. The seasonal peaks of SIC and CLD were both one month ahead of the peak in AOD. There is a strong positive correlation between AOD and SIC. Melting ice is positively correlated with chlorophyll a(CHL) almost through March to September,but negatively correlated with AOD in spring and early summer. Elevated spring and early summer AOD most likely were influenced by combination of melting ice and higher spring wind in the region. The peak of DMS flux occurred in spring due to the elevated spring wind and more melting ice. DMS concentration and AOD were positively correlated with melting ice from March to May. Elevated AOD in early autumn was likely related to the emission of biogenic aerosols associated with phytoplankton synthesis of DMS. The DMS flux would increase more than triple by 2100 in the Greenland Sea. The significant increase of biogenic aerosols could offset the warming in the Greenland Sea. | QU Bo GABRIC Albert J. ZHAO Li SUN Wenjing LI Hehe GU Peijuan JIANG Limei ZENG Meifang | 2018 | Acta Oceanologica Sinica2018，37，5： | 4 |
| 2 | Spike in phytoplankton biomass in Greenland Sea during 2009 and the correlations among chlorophyll-a,aerosol optical depth and ice cover显示文摘The distributions and correlations of chlorophyll-a(Chl-a),aerosol optical depth(AOD)and ice cover in the southeast Arctic Ocean-Greenland Sea(10°W–10°E,70°–80°N)between 2003 and 2009 were studied using satellite data and statistical analyses.Regression analysis showed correlations between Chl-a and AOD,Chl-a and ice cover,and AOD and ice cover with different time lags.The time lag of Chl-a and AOD indicated their long-term equilibrium relationship.Peaks in AOD and Chl-a and generally occurred in May and July,respectively.Despite the time lag,the correlation between Chl-a and AOD in the study region was as high as 0.7.The peak gap between Chl-a and AOD shifted for about 6 weeks during 2003–2009.In the summer and autumn of 2009,Chl-a and AOD levels were much higher than during the other years,especially in the northern band of the study region(75°–80°N).The driving forces for this localized increase in phytoplankton biomass could be mainly attributed to the very high rate of ice melting in spring and early summer and the high wind speed in autumn,together with the increased deposition of aerosol throughout the year.The unusually high AOD in the spring of 2003 was mainly due to a massive fi re in Russia,which occurred in the fi rst half of the year.Over the 7 years of the study,the sea surface temperature generally decreased.This may have been due to the release of dimethylsulfi de into the air,excreted in large amounts from abundant phytoplankton biomass,and its subsequent reaction,form large amounts of aerosol,and resulting in regional cooling. | 瞿波 Albert J. GABRIC 路海浪 林道荣 | 2014 | Chinese Journal of Oceanology and Limnology2014，32，2： | 3 |
| 3 | Using genetic algorithms to calibrate a dimethylsulfide production model in the Arctic Ocean显示文摘The global climate is intimately connected to changes in the polar oceans. The variability of sea ice coverage affects deep-water formations and large-scale thermohaline circulation patterns. The polar radiative budget is sensitive to sea-ice loss and consequent surface albedo changes. Aerosols and polar cloud microphysics are crucial players in the radioactive energy balance of the Arctic Ocean. The main biogenic source of sulfate aerosols to the atmosphere above remote seas is dimethylsulfide (DMS). Recent research suggests the flux of DMS to the Arctic atmosphere may change markedly under global warming. This paper describes climate data and DMS production (based on the five years from 1998 to 2002) in the region of the Barents Sea (30–35°E and 70–80°N). A DMS model is introduced together with an updated calibration method. A genetic algorithm is used to calibrate the chlorophyll-a (CHL) measurements (based on satellite SeaWiFS data) and DMS content (determined from cruise data collected in the Arctic). Significant interannual variation of the CHL amount leads to significant interannual variability in the observed and modeled production of DMS in the study region. Strong DMS production in 1998 could have been caused by a large amount of ice algae being released in the southern region. Forcings from a general circulation model (CSIRO Mk3) were applied to the calibrated DMS model to predict the zonal mean sea-to-air flux of DMS for contemporary and enhanced greenhouse conditions at 70–80°N. It was found that significantly decreasing ice coverage, increasing sea surface temperature and decreasing mixed-layer depth could lead to annual DMS flux increases of more than 100% by the time of equivalent CO2 tripling (the year 2080). This significant perturbation in the aerosol climate could have a large impact on the regional Arctic heat budget and consequences for global warming. | 瞿波 GABRIC J.Albert | 2010 | Chinese Journal of Oceanology and Limnology2010，28，3： | 2 |
| 4 | Correlation between sea surface temperature and wind speed in Greenland Sea and their relationships with NAO variability显示文摘The North Atlantic Oscillation (NAO) is one of the major causes of many recent changes in the Arctic Ocean. Generally, it is related to wind speed, sea surface temperature (SST), and sea ice cover. In this study, we analyzed the distributions of and correlations between SST, wind speed, NAO, and sea ice cover from 2003 to 2009 in the Greenland Sea at 10°W to 10°E, 65°N to 80°N. SST reached its peak in July, while wind speed reached its minimum in July. Seasonal variability of SST and wind speed was different for different regions. SST and wind speed mainly had negative correlations. Detailed correlation research was focused on the 75°N to 80°N band. Regression analysis shows that in this band, the variation of SST lagged three months behind that of wind speed. Ice cover and NAO had a positive correlation, and the correlation coefficient between ice cover and NAO in the year 2007 was 0.61. SST and NAO also had a positive correlation, and SST influenced NAO one month in advance. The correlation coefficients between SST and NAO reached 0.944 for the year 2005, 0.7 for the year 2008, and 0.74 for the year 2009 after shifting SST one month later. NAO also had a positive correlation with wind speed, and it also influenced wind speed one month in advance. The correlation coefficients between NAO and wind speed reached 0.783, 0.813, and 0.818 for the years 2004, 2005, and 2008, respectively, after shifting wind speed one month earlier. | Bo QU Albert J. GABRIC Jing-nan ZHU Dao-rong LIN Feng QIAN Min ZHAO | 2012 | Water Science and Engineering2012，5，3： | 2 |
| 5 | 用MODIS卫星数据来分析格陵兰海叶绿素和气溶胶光学厚度之间的关系显示文摘主要利用卫星数据MODIS Aqua研究在北极格陵兰海(10°W—10°E,70°N—85°N)2003—2009年间叶绿素a(Chl a)与气溶胶厚度(AOD)的分布以及它们之间的耦合关系。研究发现,Chl a和AOD在一定的区域里有着带有滞后期的耦合关系。同时通过统计软件EViews的滞后回归分析发现,Chl a滞后AOD三个月,Chl a和AOD之间存在着协整关系,也就是说,他们两者之间有长期的均衡关系。总体来看,Chl a从3月份开始,逐渐升高,到7月达到顶峰。AOD春天高,夏天低。Chl a和AOD在春天有较好的耦合性,相关系数达到0.98。在80°N—85°N段,除了2005年Chl a和AOD之间没有时间间隔外,其余的年份时间峰值之间的间隔有增长的趋势,7年增长了6周。AOD的峰值从原来的5月下旬前移了一个半月左右。Chl a的峰值从原来的7月下旬前移了两个月左右。2009年夏秋,在75°N—85°N,Chl a明显高于其他年份。Chl a的明显增加与高含量的AOD及大量的冰盖融化有关。 | 瞿波 路海浪 Albert Gabric 林道荣 钱峰 赵为华 | 2011 | 极地研究2011，23，1： | 2 |
| 6 | Human amnioticmembrane in the reconstruction of the ocular surface显示文摘 | Gabric N Mravicic I Dekaris I | 1999 | Doc Ophthalmol1999，98，3： | 1 |
| 7 | Profile of cytokincs in aqueous humor from corneal graft recipients显示文摘 | Dekarts I Gabric N Mazuran R Karaman Z Mravicic I | 2001 | Croat Med J2001，42，6： | 1 |
| 8 | Hmbai-eonjunetival autograft trans-plantation for recurrent pterygium显示文摘 | Dekaris Z Gabric N Karaman Z | | 0，，： | 1 |
| 9 | Hmbai-eonjunetival autograft trans-plantation for recurrent pterygium显示文摘 | Dekaris Z Gabric N Karaman Z | 2002 | Eur J Ophthalmol2002，12，1： | 1 |
| 10 | Prognostic value of visual evoked responses in childhood amblyopia显示文摘 | Henc-Petrinovic'L Deban N Gabric'N Petrinovic'J | 1993 | Eur J Ophthalm ol1993，3，3： | 1 |
| 11 | Limbal-conjunctival autograft transplantation for recurrent pterygium显示文摘 | Dekaris I Gabric N Karaman Z | 2002 | Eur J Ophthalmol2002，12，2： | 1 |
| 12 | Shelf life of packaged bakery goods: a review 显示文摘 | Galic K Curic D Gabric D | 2009 | Critical Reviews in Food Science and Nutrition2009，49，： | 1 |
| 13 | Limbal-conjunctival autograft transplantation for recurrent pterygium 显示文摘 | Dekaris I Gabric N Karaman Z | 2002 | Eur J Ophthalmol2002，12，3： | 1 |
| 14 | Limbal-conjunctival autograft transplantation for recurrent pterygium 显示文摘 | Dekaris I Gabric N Karaman Z | 2002 | Eur J Ophthalmol2002，12，3： | 1 |
| 15 | The satellite-derived distribution of chlorophyll-a and its relation to ice cover,radiation and sea surface temperature in the barents sea显示文摘 | Qu Bo Gabric A J Matrai P A | 2006 | Polar Biology2006，29，3： | 1 |
| 16 | Anti-VEGF in treatment of diabetic macular edema 显示文摘 | Boras I Lazic R Gabric N Lukic M Dekaris I | 2011 | Coll Antropol2011，35，1： | 1 |
| 17 | Coupling between ocean biota and atmospheric aerosols: dust, dimethylsulphide or artifact? 显示文摘 | Cropp R A Gabric A J McTainsh G H | 2005 | Global Biogeochemical Cycles2005，19，4： | 1 |
| 18 | Limbal-conjunctival autograft transplantation for recurrent pterygium显示文摘 | Dekaris I Gabric N Karaman Z | 2002 | Eur J Ophthalmol2002，12，3： | 1 |
| 19 | Successful primary percutaneous coronary intervention in the first trimester of pregnancy显示文摘 | Babic Z Gabric ID Pintaric H | | 0，，04： | 1 |
| 20 | The simulated response of dimethylsulphide production in the Arctic Ocean to global warming显示文摘 | Gabric A J Qu Bo Matrai P | 2005 | Tellus Series B Chemical and Physical Meteorology2005，57，5： | 1 |
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