Variation and change of upwelling dynamics detected in the world’s eastern boundary upwelling systems

dc.contributor.authorAbrahams, A
dc.contributor.authorSchlegel, R.W
dc.contributor.authorSmit, A.J
dc.date.accessioned2021-05-20T11:23:47Z
dc.date.available2021-05-20T11:23:47Z
dc.date.issued2021
dc.description.abstractGlobal increases in temperature are altering land-sea temperature gradients. Bakun (1990) hypothesized that changes within these gradients will directly affect atmospheric pressure cells associated with the development of winds and will consequently impact upwelling patterns within ecologically important Eastern Boundary Upwelling Systems (EBUS). In this study we used daily time series of NOAA Optimally Interpolated sea surface temperature (SST) and ERA 5 reanalysis wind products to calculate a series novel of metrics related to upwelling dynamics. We then use these to objectively describe upwelling signals in terms of their frequency, intensity and duration throughout the four EBUS during summer months over the last 37 years (1982–2019). We found that a decrease (increase) in SST is associated with an increase (decrease) in the number of upwelling “events,” a decrease (increase) in the intensity of upwelling, and an increase (decrease) in the cumulative intensity of upwelling, with differences between EBUS and regions within EBUS.en_US
dc.identifier.citationAbrahams, A. et al. (2021). Variation and change of upwelling dynamics detected in the world’s eastern boundary upwelling systems. Frontiers in Marine Science, 8,626411en_US
dc.identifier.issn2296-7745
dc.identifier.uri10.3389/fmars.2021.626411
dc.identifier.urihttp://hdl.handle.net/10566/6176
dc.language.isoenen_US
dc.publisherFrontiers Media S.A.en_US
dc.subjectClimate changeen_US
dc.subjectCoastal regionsen_US
dc.subjectRemotely sensed SSTen_US
dc.subjectSeawater temperatureen_US
dc.subjectUpwellingen_US
dc.titleVariation and change of upwelling dynamics detected in the world’s eastern boundary upwelling systemsen_US
dc.typeArticleen_US

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