Relevant bibliographies by topics / Phytoplankton spring bloom

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  1. Journal articles
  2. Dissertations / Theses
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  4. Book chapters
  5. Conference papers

Academic literature on the topic 'Phytoplankton spring bloom'

Author: Grafiati
Published: 2 June 2025
Last updated: 31 July 2025

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Journal articles on the topic "Phytoplankton spring bloom"

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Lewandowska, Aleksandra M., Maren Striebel, Ulrike Feudel, Helmut Hillebrand, and Ulrich Sommer. "The importance of phytoplankton trait variability in spring bloom formation." ICES Journal of Marine Science 72, no. 6 (2015): 1908–15. http://dx.doi.org/10.1093/icesjms/fsv059.

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Abstract About 60 years ago, the critical depth hypothesis was proposed to describe the occurrence of spring phytoplankton blooms and emphasized the role of stratification for the timing of onset. Since then, several alternative hypotheses appeared focusing on the role of grazing and mixing processes such as turbulent convection or wind activity. Surprisingly, the role of community composition—and thus the distribution of phytoplankton traits—for bloom formation has not been addressed. Here, we discuss how trait variability between competing species might influence phytoplankton growth during
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Waga, Hisatomo, Hajo Eicken, Toru Hirawake, and Yasushi Fukamachi. "Variability in spring phytoplankton blooms associated with ice retreat timing in the Pacific Arctic from 2003–2019." PLOS ONE 16, no. 12 (2021): e0261418. http://dx.doi.org/10.1371/journal.pone.0261418.

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The Arctic is experiencing rapid changes in sea-ice seasonality and extent, with significant consequences for primary production. With the importance of accurate monitoring of spring phytoplankton dynamics in a changing Arctic, this study further examines the previously established critical relationship between spring phytoplankton bloom types and timing of the sea-ice retreat for broader temporal and spatial coverages, with a particular focus on the Pacific Arctic for 2003–2019. To this end, time-series of satellite-retrieved phytoplankton biomass were modeled using a parametric Gaussian func
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Mignot, A., R. Ferrari, and K. A. Mork. "Spring bloom onset in the Nordic Seas." Biogeosciences Discussions 12, no. 16 (2015): 13631–73. http://dx.doi.org/10.5194/bgd-12-13631-2015.

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Abstract. The North Atlantic spring bloom is a massive annual growth event of marine phytoplankton, tiny free-floating algae that form the base of the ocean's food web and generates a large fraction of the global primary production of organic matter. The conditions that trigger the onset of the spring bloom in the Nordic Seas, at the northern edge of the North Atlantic, are studied using in-situ data from five bio-optical floats released above the Arctic Circle. It is often assumed that spring blooms start as soon as phytoplankton cells daily irradiance is sufficiently abundant that division r
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Mignot, Alexandre, Raffaele Ferrari, and Kjell Arne Mork. "Spring bloom onset in the Nordic Seas." Biogeosciences 13, no. 11 (2016): 3485–502. http://dx.doi.org/10.5194/bg-13-3485-2016.

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Abstract. The North Atlantic spring bloom is a massive annual growth event of marine phytoplankton, tiny free-floating algae that form the base of the ocean's food web and generates a large fraction of the global primary production of organic matter. The conditions that trigger the onset of the spring bloom in the Nordic Seas, at the northern edge of the North Atlantic, are studied using in situ data from six bio-optical floats released north of the Arctic Circle. It is often assumed that spring blooms start as soon as phytoplankton cells daily irradiance is sufficiently abundant that division
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Корсак, M. Korsak, Мошаров, et al. "Influence of Solar Physics Factors on the Spring Growth of Phytoplankton in Reservoir." Safety in Technosphere 6, no. 2 (2017): 19–27. http://dx.doi.org/10.12737/article_598d6e6af0ec46.94857569.

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The article gives the results of retrospective statistical analysis, which justify the presence of statistical dependencies between the dates of the beginning and the peak values of the spring phytoplankton bloom in the Uchinsk reservoir and the intensity of total solar radiation in the range of photosynthetically active radiation (PAR), as well as the value of the integral indices of the activity of the Sun (Wolf number), in the period preceding of phytoplankton bloom. It is found, that the greater the magnitude of the fluxes of solar radiation in the PAR range will get the surface of the res
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Ferreira, Afonso, Vanda Brotas, Carla Palma, Carlos Borges, and Ana C. Brito. "Assessing Phytoplankton Bloom Phenology in Upwelling-Influenced Regions Using Ocean Color Remote Sensing." Remote Sensing 13, no. 4 (2021): 675. http://dx.doi.org/10.3390/rs13040675.

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Phytoplankton bloom phenology studies are fundamental for the understanding of marine ecosystems. Mismatches between fish spawning and plankton peak biomass will become more frequent with climate change, highlighting the need for thorough phenology studies in coastal areas. This study was the first to assess phytoplankton bloom phenology in the Western Iberian Coast (WIC), a complex coastal region in SW Europe, using a multisensor long-term ocean color remote sensing dataset with daily resolution. Using surface chlorophyll a (chl-a) and biogeophysical datasets, five phenoregions (i.e., areas w
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Mahadevan, Amala, Eric D’Asaro, Craig Lee, and Mary Jane Perry. "Eddy-Driven Stratification Initiates North Atlantic Spring Phytoplankton Blooms." Science 337, no. 6090 (2012): 54–58. http://dx.doi.org/10.1126/science.1218740.

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Springtime phytoplankton blooms photosynthetically fix carbon and export it from the surface ocean at globally important rates. These blooms are triggered by increased light exposure of the phytoplankton due to both seasonal light increase and the development of a near-surface vertical density gradient (stratification) that inhibits vertical mixing of the phytoplankton. Classically and in current climate models, that stratification is ascribed to a springtime warming of the sea surface. Here, using observations from the subpolar North Atlantic and a three-dimensional biophysical model, we show
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Record, Nicholas R., William M. Balch, and Karen Stamieszkin. "Century-scale changes in phytoplankton phenology in the Gulf of Maine." PeerJ 7 (May 2, 2019): e6735. http://dx.doi.org/10.7717/peerj.6735.

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The phenology of major seasonal events is an important indicator of climate. We analyzed multiple datasets of in situ chlorophyll measurements from the Gulf of Maine dating back to the early 20th century in order to detect climate-scale changes in phenology. The seasonal cycle was consistently characterized by a two-bloom pattern, with spring and autumn blooms. The timing of both spring and autumn blooms has shifted later in the year at rates ranging from ∼1 to 9 days per decade since 1960, depending on the phenology metric, and trends only emerged at time scales of >40 years. Bloom phenolo
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Miladinova, Svetla, Adolf Stips, Diego Macias Moy, and Elisa Garcia-Gorriz. "Seasonal and Inter-Annual Variability of the Phytoplankton Dynamics in the Black Sea Inner Basin." Oceans 1, no. 4 (2020): 251–73. http://dx.doi.org/10.3390/oceans1040018.

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We explore the patterns of Black Sea phytoplankton growth as driven by the thermohaline structure and circulation system and the freshwater nutrient loads. Seasonal and inter-annual variability of the phytoplankton blooms is examined using hydrodynamic simulations that resolve mesoscale eddies and online coupled bio-geochemical model. This study suggests that the bloom seasonality is homogeneous across geographic locations of the Black Sea inner basin, with the strongest bloom occurring in winter (February–March), followed by weaker bloom in spring (April–May), summer deep biomass maximum (DBM
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Brody, Sarah R., and M. Susan Lozier. "Characterizing upper-ocean mixing and its effect on the spring phytoplankton bloom with in situ data." ICES Journal of Marine Science 72, no. 6 (2015): 1961–70. http://dx.doi.org/10.1093/icesjms/fsv006.

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Abstract Since publication, the Sverdrup hypothesis, that phytoplankton are uniformly distributed within the ocean mixed layer and bloom once the ocean warms and stratifies in spring, has been the conventional explanation of subpolar phytoplankton spring bloom initiation. Recent studies have sought to differentiate between the actively mixing section of the upper ocean and the uniform-density mixed layer, arguing, as Sverdrup implied, that decreases in active mixing drive the spring bloom. In this study, we use in situ data to investigate the characteristics and depth of active mixing in both
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Dissertations / Theses on the topic "Phytoplankton spring bloom"

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Hemmings, John Christopher Paul. "Quantitative modelling of spatial variability in the north Atlantic spring phytoplankton bloom." Thesis, University of Southampton, 1999. https://eprints.soton.ac.uk/42095/.

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The effects of variability in the physical environment on the development of the spring phytoplankton bloom are investigated using a physically forced model of the annual plankton cycle in the ocean mixed layer. The model is optimised to fit survey data from the eastern North Atlantic, collected over a 1500 x 1500 km area between 39N and 54N, from April-June 1991, establishing the feasibility of using spatially distributed point-in-time data in model calibration. Measurements made below the seasonal pycnocline show the existence of an empirical relationship between preformed nitrate and salini
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Wolfe, Megan Amelia. "Impact of wind and river flow on the timing of the Rivers Inlet spring phytoplankton bloom." Thesis, University of British Columbia, 2010. http://hdl.handle.net/2429/27081.

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The primary objective of this masters study is to develop an understanding of the physical processes driving the timing of the spring phytoplankton bloom in Rivers Inlet. The spring bloom is initiated as light limitation is lifted causing an increase in growth which overcomes loses due to grazing and advection. The bloom is terminated by nitrate exhaustion. The physical system can impact the spring bloom through variations of winds, cloud coverage, and river input. Strong winds showed two effects. First, strong winds increased the mixing layer depth which decreased the amount of light avail
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Bárbulo, Diego. "Influence of sea ice seeding on the spring phytoplankton bloom : An experimental study in the Gulf of Bothnia." Thesis, Umeå universitet, Institutionen för ekologi, miljö och geovetenskap, 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:umu:diva-148586.

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The influence of sea ice seeding on the northern Baltic Sea´s pelagic phytoplankton spring bloom was studied in a laboratory experiment in which microcosms mimicked sea conditions. On March 26th, 2018, samples (ice cores and seawater) were taken from land-fast ice at a coastal station in the Gulf of Bothnia. The seeding experiment lasted for 9 days, during which a 12:12 hours light:dark incubation took place. Four different treatments (two with ice and two without it) were set up in twelve incubated microcosms. Samples for analyses were taken on days 0, 3, 6 and 9. On day 0, measurements were
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Schock, Kevin A. "An analysis of a persistent isotherm tilt during early-spring and its effect on the diatom bloom : Lake Washington, Seattle, WA /." Thesis, Connect to this title online; UW restricted, 2008. http://hdl.handle.net/1773/10177.

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Luengen, Allison Christine. "Investigating the spring bloom in San Francisco Bay : links between water chemistry, metal cycling, mercury speciation, and phytoplankton community composition /." Diss., Digital Dissertations Database. Restricted to UC campuses, 2007. http://uclibs.org/PID/11984.

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Hobbs, Erin B. "Distribution and feeding behavior of early life stages of the northern shrimp, Pandalus borealis, in relation to the spring phytoplankton bloom in the western Gulf of Maine /." Restricted access (UM), 2008. http://libraries.maine.edu/gateway/oroauth.asp?file=orono/etheses/37803141.pdf.

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Louchart, Arnaud. "Dynamique spatio-temporelle des communautés phytoplanctoniques côtières et de leurs caractéristiques intrinsèques, à partir d'une approche automatisée à haute résolution Phytoplankton distribution from Western to Central English Channel, revealed by automated flow cytometry during the summer-fall transition Spatial niches of phytoplankton functional groups assessed during a spring bloom development in two temperate coastal seas Untangling the vertical distribution of phytoplankton groups along a salinity gradient through the Baltic Sea and the Skagerrak-Kattegat straits." Thesis, Littoral, 2020. http://www.theses.fr/2020DUNK0556.

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Au sein des écosystèmes côtiers, la composition, la distribution et la dynamique phytoplanctoniques sont influencées par les variations spatio-temporelles des structures hydrologiques et des para mètres biogéochimiques, sous les pressions naturelles et anthropiques. Les suivis de référence, de par leur faible résolution spatiale et temporelle, peuvent manquer des événements-clés comme l'initiation ou la fin des efflorescences ou nuisibles (du type Harmful Algal Blooms). Pour permettre leur détection et mieux comprendre la distribution et la dynamique de ce compartiment à la base des réseaux tr
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Seward, Lindsay C. N. "The Relationship between Green Sea Urchin Spawning, Spring Phytoplankton Blooms, and the Winter-Spring Hydrography at Selected Sites in Maine." Fogler Library, University of Maine, 2002. http://www.library.umaine.edu/theses/pdf/SewardLCN2002.pdf.

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Ji, Rubao. "Biological and physical processes controlling the spring phytoplankton bloom dynamics on Georges Bank." 2003. http://purl.galileo.usg.edu/uga%5Fetd/ji%5Frubao%5F200312%5Fphd.

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Brody, Sarah. "Physical Drivers of the Spring Phytoplankton Bloom in the Subpolar North Atlantic Ocean." Diss., 2015. http://hdl.handle.net/10161/9850.

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<p>The timing of the spring phytoplankton bloom in the subpolar North Atlantic Ocean has important consequences for the marine carbon cycle and ecosystems. There are currently several proposed mechanisms to explain the timing of this bloom. The conventional theory holds that the bloom begins when the ocean warms and the seasonal mixed layer shoals in the spring, decreasing the depth to which phytoplankton are mixed and increasing the light available to the population. Recent work has attributed the beginning of the bloom to decreases in turbulence within the upper ocean, driven by the onset
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Books on the topic "Phytoplankton spring bloom"

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Walsh, John Joseph. Satellite detection of phytoplankton export from the Mid-Atlantic Bight during the 1979 spring bloom. National Aeronautics and Space Administration, 1986.

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Book chapters on the topic "Phytoplankton spring bloom"

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Dahl, Einar, Odd Lindahl, Eystein Paasche, and Jahn Throndsen. "The Chrysochromulina polylepis Bloom in Scandinavian Waters During Spring 1988." In Novel Phytoplankton Blooms. Springer Berlin Heidelberg, 1989. http://dx.doi.org/10.1007/978-3-642-75280-3_23.

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Zheng, Xiaoshen, and Hao Wei. "Analysis of Chlorophyll Concentration during the Phytoplankton Spring Bloom in the Yellow Sea Based on the MODIS Data." In Lecture Notes in Computer Science. Springer Berlin Heidelberg, 2010. http://dx.doi.org/10.1007/978-3-642-15615-1_31.

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Cloern, James E., and Alan D. Jassby. "Year-to-Year Fluctuation of the Spring Phytoplankton Bloom in South San Francisco Bay: An Example of Ecological Variability at the Land-Sea Interface." In Ecological Time Series. Springer US, 1995. http://dx.doi.org/10.1007/978-1-4615-1769-6_10.

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Cloern, James E., and Alan D. Jassby. "Year-to-Year Fluctuation of the Spring Phytoplankton Bloom in South San Francisco Bay: An Example of Ecological Variability at the Land-Sea Interface." In Ecological Time Series. Springer US, 1995. http://dx.doi.org/10.1007/978-1-4615-6881-0_10.

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Hamed, Adel F., Rehab M. Mohamed, and Wiame W. Emam. "Potentiality of Remote Sensing for Monitoring Phytoplankton Bloom." In Springer Remote Sensing/Photogrammetry. Springer Nature Switzerland, 2025. https://doi.org/10.1007/978-3-031-78768-3_7.

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Mulyadi, Hanung Agus, Arief Rachman, and Nurul Fitriya. "Zooplankton Response to Harmful Algae Blooms (HABs) Species Phytoplankton." In Springer Proceedings in Physics. Springer Nature Singapore, 2023. http://dx.doi.org/10.1007/978-981-19-9768-6_43.

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Martinez, Elodie, David Antoine, Fabrizio D’Ortenzio, and Clement DeBoyerMontégut. "DecPhy—Variability of the Phytoplankton Spring and Fall Blooms in the Northeastern Atlantic in the 1980s and 2000s." In SpringerBriefs in Earth System Sciences. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-32521-2_6.

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Allen, J. I. "Simulating the spring phytoplankton bloom in the Humber Plume (UK) with a variable phytoplankton carbon: chlorophyll-a model." In Opertional Oceanography - Implementation at the European and Regional Scales, Proceedings of the second international Conference on EuroGOOS. Elsevier, 2002. http://dx.doi.org/10.1016/s0422-9894(02)80056-3.

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Gray, John S., and Michael Elliott. "Temporal variations in benthic assemblages." In Ecology of Marine Sediments. Oxford University Press, 2009. http://dx.doi.org/10.1093/oso/9780198569015.003.0011.

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Most (but by no means all) benthic species have larval stages which use the water column for dispersal. As indicated in the previous chapter, a key process affecting recruitment to sediment systems is the need to disperse larvae in order to colonize new areas, even to the extent of releasing larvae at spring tides when the tidal excursion will be greatest, thus effecting an even greater dispersal. Seasonal release of larvae is the norm: most species develop gametes in spring and spawn in late spring or early summer (see Rasmussen 1973 for an excellent data set of the times of planktonic larval
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Conference papers on the topic "Phytoplankton spring bloom"

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Weeks, Alison R., Ian S. Robinson, James Aiken, and G. F. Moore. "Maintaining a phytoplankton bloom in low mixed layer illumination in the Bellinghausen Sea in the Austral Spring, 1992." In Ocean Optics XII, edited by Jules S. Jaffe. SPIE, 1994. http://dx.doi.org/10.1117/12.190035.

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Eilertsen, Hans-Christian, Geir A. Hansen, Harald Svendsen, and Else N. Hegseth. "Onset of the spring phytoplankton bloom in the Barents Sea: influence of changing light regime and other environmental factors." In High Latitude Optics, edited by Hans-Christian Eilertsen. SPIE, 1993. http://dx.doi.org/10.1117/12.165507.

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Podymov, O., O. Podymov, N. Kuzevanova, N. Kuzevanova, A. Khvorosch, and A. Khvorosch. "LONG-TERM MONITORING OF SEASONAL AND INTERANNUAL VARIABILITY OF HYDROLOGICAL STRUCTURE IN COASTAL ZONE OF THE NORTH-EASTERN BLACK SEA." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b93b554e1b8.09734764.

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The work demonstrates the results of the 6-years complex ship-borne monitoring of coastal zone in the north-eastern part of the Black Sea, carried out by the Southern Branch of P.P.Shirshov Institute of Oceanology, RAS, on a marine cross-section at the Blue Bay (Gelendzhik) beam 1-2 times per month. Climatic changes and eutrophication exert a significant impact on the sea water at the coastal area. In case of the Black Sea these factors pile up with a permanent hydrogen sulphide contamination of the sea water below 80-200 meters depth (depending on the season and distance from the shore). Stro
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Podymov, O., O. Podymov, N. Kuzevanova, N. Kuzevanova, A. Khvorosch, and A. Khvorosch. "LONG-TERM MONITORING OF SEASONAL AND INTERANNUAL VARIABILITY OF HYDROLOGICAL STRUCTURE IN COASTAL ZONE OF THE NORTH-EASTERN BLACK SEA." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b4317195e3a.

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The work demonstrates the results of the 6-years complex ship-borne monitoring of coastal zone in the north-eastern part of the Black Sea, carried out by the Southern Branch of P.P.Shirshov Institute of Oceanology, RAS, on a marine cross-section at the Blue Bay (Gelendzhik) beam 1-2 times per month. Climatic changes and eutrophication exert a significant impact on the sea water at the coastal area. In case of the Black Sea these factors pile up with a permanent hydrogen sulphide contamination of the sea water below 80-200 meters depth (depending on the season and distance from the shore). Stro
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