Karin Kvale

ORCID: 0000-0001-8043-5431
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About
Contact & Profiles
Research Areas
  • Marine and coastal ecosystems
  • Microplastics and Plastic Pollution
  • Geology and Paleoclimatology Research
  • Marine Biology and Ecology Research
  • Ocean Acidification Effects and Responses
  • Methane Hydrates and Related Phenomena
  • Oceanographic and Atmospheric Processes
  • Atmospheric and Environmental Gas Dynamics
  • Microbial Community Ecology and Physiology
  • Paleontology and Stratigraphy of Fossils
  • Recycling and Waste Management Techniques
  • Coastal and Marine Management
  • Diatoms and Algae Research
  • Effects and risks of endocrine disrupting chemicals
  • Geomagnetism and Paleomagnetism Studies
  • Geological formations and processes
  • Science, Research, and Medicine
  • Climate variability and models
  • Isotope Analysis in Ecology
  • Marine Bivalve and Aquaculture Studies
  • Species Distribution and Climate Change
  • Ecosystem dynamics and resilience
  • Healthcare Systems and Challenges
  • Biotechnology and Related Fields
  • Mercury impact and mitigation studies

GNS Science
2021-2024

GEOMAR Helmholtz Centre for Ocean Research Kiel
2015-2024

University of Tasmania
2023

UNSW Sydney
2011-2016

ARC Centre of Excellence for Climate System Science
2014-2015

University of Victoria
2012

Indiana University
2006

Dartmouth College
2000

Abstract Global warming has driven a loss of dissolved oxygen in the ocean recent decades. We demonstrate potential for an additional anthropogenic driver deoxygenation, which zooplankton consumption microplastic reduces grazing on primary producers. In regions where production is not limited by macronutrient availability, reduction pressure producers causes export to increase. Consequently, organic particle remineralisation these increases. Employing comprehensive Earth system model...

10.1038/s41467-021-22554-w article EN cc-by Nature Communications 2021-04-21

Abstract Every year, about four percent of the plastic waste generated worldwide ends up in ocean. What happens to there is poorly understood, though a growing body evidence suggests it rapidly spreading throughout global The mechanisms this spread are straightforward for buoyant larger plastics that can be accurately modelled using Lagrangian particle models. But fate smallest size fractions (the microplastics) less straightforward, part because they aggregate sinking marine snow and faecal...

10.1038/s41598-020-72898-4 article EN cc-by Scientific Reports 2020-10-07

Numerical simulations and emissions estimates of plastic in to the ocean consistently over-predict surface inventory, particularly case microplastic (MP), i.e. fragments less than 5 mm length. Sequestration sediments has been both predicted and, a limited extent, observed. It hypothesized that biology may be exporting significant fraction MP by way marine snow aggregation zooplankton faecal pellets. We apply previously published data on concentrations an earth system model intermediate...

10.3389/fmars.2019.00808 article EN cc-by Frontiers in Marine Science 2020-01-21

Abstract The marine biological carbon pump (BCP) stores in the ocean interior, isolating it from exchange with atmosphere and thereby coregulating atmospheric dioxide (CO 2 ). As BCP commonly is equated flux of organic material to termed “export flux,” a change export perceived directly impact CO , thus climate. Here, we recap how this perception contrasts current understanding BCP, emphasizing lack direct relationship between global . We argue for use storage origin interior as diagnostic...

10.1111/gcb.17124 article EN cc-by Global Change Biology 2024-01-01

Abstract. Global biogeochemical ocean models are often tuned to match the observed distributions and fluxes of inorganic organic quantities. This tuning is typically carried out “by hand”. However, this rather subjective approach might not yield best fit observations, closely linked circulation employed thus influenced by its specific features even faults. We here investigate effect model tuning, via objective optimisation, one intermediate complexity when simulated in five different offline...

10.5194/bg-17-3057-2020 article EN cc-by Biogeosciences 2020-06-18

Abstract Climate change and plastics pollution are dual threats to marine environments. Here we use biogeochemical microplastic modelling show that even if there is complete removal of microplastics cessation deposition in the oceans 2022, regional recovery from microplastic-induced remineralization water column deoxygenation could take hundreds years for coastal upwelling zones, North Pacific Southern Ocean. Surface stratification reduced sea ice cover further impede recovery, highlighting...

10.1038/s41561-022-01096-w article EN cc-by Nature Geoscience 2022-12-22

Abstract Scientific research over the past decade has demonstrated that plastic in our oceans detrimental consequences for marine life at all trophic levels. As countries negotiate an international legally binding instrument on pollution, focus is eliminating emissions to environment. Here, we argue that, while this endeavour urgently needed limit negative impacts of ocean ecosystems, reduction flow environment should not be sole purpose negotiations. Legacy oceanic pollution also a major...

10.1186/s43591-023-00074-2 article EN cc-by Microplastics and Nanoplastics 2023-11-13

The sea surface microlayer (SML) refers to the uppermost millimeter of ocean that is in direct contact with atmosphere. It has physicochemical and biological properties are distinct from underlying water its determine air-sea exchange momentum, mass energy. Gas transfer velocity mostly determined by wind forcing, where gas enhanced at low moderate speeds. However, pollutant enrichment SML surfactants reduces suppressing turbulence damping waves. Local impacts can be significant, reducing...

10.5194/egusphere-egu25-7269 preprint EN 2025-03-14

Abstract As climate change continues, the likelihood of passing critical thresholds or tipping points increases. Hence, there is a need to advance science for detecting such thresholds. In this paper, we assess needs and opportunities Earth Observation (EO, here understood refer satellite observations) inform society in responding risks associated with ten potential large-scale ocean elements: Atlantic Meridional Overturning Circulation; Subpolar Gyre; Beaufort Arctic halocline; Kuroshio...

10.1007/s10712-024-09859-3 article EN cc-by Surveys in Geophysics 2024-11-06

Microplastic is a ubiquitous marine pollutant whose small dimensions make it biologically available to phytoplankton and zooplankton. These organisms are crucial as the basis of food web for export organic material in form faecal pellets from surface deeper water column, forming long-term carbon sink. Previous laboratory studies have demonstrated empirically that ingestion low density microplastics reduces sinking rates zooplankton pellets. This study uses complex earth system model analyse...

10.3389/fmars.2023.1111838 article EN cc-by Frontiers in Marine Science 2023-02-09

Autotrophy is largely resource-limited in the modern ocean. Paleo evidence indicates this was not necessarily case warmer climates, and observations as well standard metabolic theory suggest continued ocean warming could shift global ecology towards heterotrophy, thereby reducing autotrophic nutrient limitation. Such a would entail strong recycling upper high rates of net primary production (NPP), yet low carbon export to deep sediments. We demonstrate transition such state early 22nd...

10.1088/1748-9326/10/7/074009 article EN cc-by Environmental Research Letters 2015-07-01

Marine calcifiers as a plankton functional type (PFT) are crucial part of the global carbon cycle, being responsible for much export to deep ocean entering via biological pathways. Deep through is controlled by physiological, ecological, and biogeochemical factors. This paper describes implementation calcifying phytoplankton PFT in University Victoria Earth System Climate Model, version 2.9 (UVic ESCM), mechanistic improvements representation model (a full calcite tracer, carbonate chemistry...

10.1080/07055900.2015.1049112 article EN ATMOSPHERE-OCEAN 2015-05-27

Plastic pollution can both chemically and physically impede marine biota. But it also provide novel substrates for colonization, its leachate might stimulate phytoplankton growth. contains carbon, which is released into the environment upon breakdown. All of these mechanisms have been proposed to contribute global impacts on open ocean carbon cycling climate from ubiquitous plastic pollution. Laboratory studies produce compelling data showing stimulation inhibition primary producers...

10.1042/etls20220013 article EN Emerging Topics in Life Sciences 2022-10-11

The Global Plastics Treaty presents an opportunity to "end plastic pollution". Legacy plastics will continue fragment secondary microplastics for decades, without additional mitigation measures. We identify this flux as a "fragmentation gap", currently overlooked in global policy targets.

10.1038/s41467-024-53962-3 article EN cc-by-nc-nd Nature Communications 2024-11-13

Abstract. Treatment of the underwater light field in ocean biogeochemical models has been attracting increasing interest, with some moving towards more complex parameterisations. We conduct a simple sensitivity study typical, highly simplified parameterisation. In our study, we vary phytoplankton attenuation parameter over range constrained by data during both pre-industrial equilibrated and future climate scenario RCP8.5. equilibrium, lower parameters (weaker self-shading) shift net primary...

10.5194/bg-14-4767-2017 article EN cc-by Biogeosciences 2017-10-25

Abstract. Conventional integration of Earth system and ocean models can accrue considerable computational expenses, particularly for marine biogeochemical applications. Offline numerical schemes in which only the tracers are time stepped transported using a pre-computed circulation field substantially reduce burden thus an attractive alternative. One such scheme is transport matrix method (TMM), represents tracer as sequence sparse matrix–vector products that be performed efficiently on...

10.5194/gmd-10-2425-2017 article EN cc-by Geoscientific model development 2017-06-29

Abstract Phytoplankton exert a significant control on the marine carbon cycle and can thus impact atmospheric CO 2 concentration. Here we use new ecosystem model to analyze response of diatoms coccolithophores in Southern Ocean Last Glacial Maximum (LGM) climate conditions, changes aeolian iron (Fe) input Ocean. We find that LGM conditions without Fe lead large increase north winter sea ice edge South Atlantic (19%) Pacific (26%), 31% 9% within seasonal sea‐ice zone Indian oceans,...

10.1029/2020pa004075 article EN publisher-specific-oa Paleoceanography and Paleoclimatology 2021-07-01

Since the beginning of its large-scale production in early 20th century, plastics have remained an important material widespread use throughout modern society. Nevertheless, despite possessing many benefits, are resistant to degradation and instead accumulate ocean terrestrial sediments, thereby potentially affecting marine ecosystems. Plastics release CO 2 their entire lifecycle; during extraction materials used production, through plastic–carbon leaching environment, different end-of-life...

10.1139/facets-2023-0061 article EN cc-by FACETS 2023-01-01

Abstract Microplastics are ubiquitous in marine environments and can be incorporated into biological aggregates including snows faecal pellets. These suspected to a major removal mechanism for microplastics from the surface ocean, transporting them deeper levels seafloor as they sink remineralise. However, simple budget calculations, observations, model parameter testing suggest that aggregation might also lead retention of upper sustaining contamination biologically-productive environments....

10.1088/1748-9326/ad472c article EN cc-by Environmental Research Letters 2024-05-03

Abstract. Phytoplankton calcifiers contribute to global carbon cycling through their dual formation of calcium carbonate and particulate organic (POC). The might provide an efficient export pathway for the associated POC deep ocean, reducing particles' exposure biological degradation in upper ocean increasing particle settling rate. Previous work has suggested ballasting by increase a warming climate, spite dissolution rates, because benefit from widespread nutrient limitation arising...

10.5194/bg-16-1019-2019 article EN cc-by Biogeosciences 2019-03-14

Abstract Antarctic ice core records suggest that atmospheric CO 2 increased by 15–20 ppm during Heinrich stadials (HS). These periods of abrupt increase are associated with a significant weakening the Atlantic meridional overturning circulation (AMOC), and warming at high southern latitudes. As such, modeling studies have explored link between changes in AMOC, latitude climate . While proxy aeolian iron input to Southern Ocean decreased significantly HS, potential impact on reduced combined...

10.1029/2023pa004754 article EN cc-by Paleoceanography and Paleoclimatology 2024-02-01

Abstract. We describe and test a new model of biological marine silicate cycling, implemented in the University Victoria Earth System Climate Model (UVic ESCM) version 2.9. This adds diatoms, which are key aspect carbon pump, to an existing ecosystem model. The performs well against important ocean biogeochemical indicators captures large-scale features silica cycle. Furthermore it is computationally efficient, allowing both fully-coupled, long-timescale transient simulations, as "offline"...

10.5194/gmd-2020-235 preprint EN cc-by 2020-09-09
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