01001nam a2200265 i 450099100106776970753620020507182620.0950911s1980 de ||| | eng 3540087745b10796447-39ule_instLE01306536ExLDip.to Matematicaeng519.4AMS 65P05Glowinski, Roland41336Lectures on numerical methods for non-linear variational problems /by R. GlowinskiBerlin :Springer-Verlag,1980vii, 240 p. ;24 cm.Partial differential equations-miscellaneous topics.b1079644721-09-0628-06-02991001067769707536LE013 65P05 GLO11 (1980)12013000034805le013-E0.00-l- 00000.i1089794x28-06-02Lectures on Numerical Methods for Non Linear Variational Problems381220UNISALENTOle01301-01-95ma -engde 0104183nam 2201021z- 450 991058594360332120220812(CKB)5600000000483044(oapen)https://directory.doabooks.org/handle/20.500.12854/91125(oapen)doab91125(EXLCZ)99560000000048304420202208d2022 |y 0engurmn|---annantxtrdacontentcrdamediacrrdacarrierMarine Nitrogen Fixation and Phytoplankton EcologyBaselMDPI - Multidisciplinary Digital Publishing Institute20221 online resource (208 p.)3-0365-4667-7 3-0365-4668-5 Many oceans are currently undergoing rapid changes in environmental conditions such as warming temperature, acidic water condition, coastal hypoxia, etc. These changes could lead to dramatic changes in the biology and ecology of phytoplankton and consequently impact the entire marine ecosystems and global biogeochemical cycles. Marine phytoplankton can be an important indicator for the changes in marine environments and ecosystems since they are major primary producers that consolidate solar energy into various organic matter transferred to marine ecosystems throughout the food-webs. Similarly, the N2 fixers (diazotrophs) are also vulnerable to changing environmental conditions. It has been found that the polar regions can be introduced to diazotrophic activity under warming conditions and the increased N availability can lead to elevated primary productivity. Considering the fundamental roles of phytoplankton in marine ecosystems and global biogeochemical cycles, it is important to understand phytoplankton ecology and N2 fixation as a potential N source in various oceans. This Special Issue provides ecological and biogeochemical baselines in a wide range of geographic study regions for the changes in marine environments and ecosystems driven by global climate changes.Environmental economicsbicsscResearch and information: generalbicsscArctic OceanBering Seabiochemical compositionbiochemical compositionsbiovolumeCanada Basincarbohydratescarbon and nitrogenchlorophyll achlorophyll-aChukchi SeaChukchi ShelfcyanobacteriadiatomdiatomsEast China Seaeddyfood materialHeterosigma akashiwoHPLCJaran BayKongsfjordenlipidsmacromolecular compositionmacromoleculesn/anorthwestern Pacific Oceanparticulate organic carbonparticulate organic matterparticulate organic nitrogenphytoplanktonphytoplankton productivityPOCpolar nightprimary productionprimary productivityProchlorococcusproteinsRhizosolenia-RicheliaRoss SeaScrippsiella trochoideasmall phytoplanktonSouth China Seastable isotopesSvalbardSynechococcusTEPTEP-Ctransparent exopolymer particlesTrichodesmiumupwellingEnvironmental economicsResearch and information: generalLee Sang Heonedt884501Bhavya P.SedtKim Bo KyungedtLee Sang HeonothBhavya P.SothKim Bo KyungothBOOK9910585943603321Marine Nitrogen Fixation and Phytoplankton Ecology3031742UNINA