@article{McLoughlinPalmerMakeigetal.2017,
  author    = {McLoughlin, Grainne and Palmer, Jason and Makeig, Scott and Bigdely-Shamlo, Nima and Banaschewski, Tobias and Laucht, Manfred and Brandeis, D.},
  title     = {EEG Source Imaging Indices of Cognitive Control Show Associations with Dopamine System Genes},
  series = {Brain Topography},
  volume    = {31},
  journal   = {Brain Topography},
  number    = {3},
  publisher = {Springer},
  address   = {Dordrecht},
  issn      = {0896-0267},
  doi       = {10.1007/s10548-017-0601-z},
  pages     = {392 -- 406},
  year      = {2017},
  abstract  = {Cognitive or executive control is a critical mental ability, an important marker of mental illness, and among the most heritable of neurocognitive traits. Two candidate genes, catechol-O-methyltransferase (COMT) and DRD4, which both have a roles in the regulation of cortical dopamine, have been consistently associated with cognitive control. Here, we predicted that individuals with the COMT Met/Met allele would show improved response execution and inhibition as indexed by event-related potentials in a Go/NoGo task, while individuals with the DRD4 7-repeat allele would show impaired brain activity. We used independent component analysis (ICA) to separate brain source processes contributing to high-density EEG scalp signals recorded during the task. As expected, individuals with the DRD4 7-repeat polymorphism had reduced parietal P3 source and scalp responses to response (Go) compared to those without the 7-repeat. Contrary to our expectation, the COMT homozygous Met allele was associated with a smaller frontal P3 source and scalp response to response-inhibition (NoGo) stimuli, suggesting that while more dopamine in frontal cortical areas has advantages in some tasks, it may also compromise response inhibition function. An interaction effect emerged for P3 source responses to Go stimuli. These were reduced in those with both the 7-repeat DRD4 allele and either the COMT Val/Val or the Met/Met homozygous polymorphisms but not in those with the heterozygous Val/Met polymorphism. This epistatic interaction between DRD4 and COMT replicates findings that too little or too much dopamine impairs cognitive control. The anatomic and functional separated maximally independent cortical EEG sources proved more informative than scalp channel measures for genetic studies of brain function and thus better elucidate the complex mechanisms in psychiatric illness.},
  language  = {en}
}
@misc{PalmerGregoryBaggeetal.2020,
  author    = {Palmer, Matthew D. and Gregory, Jonathan and Bagge, Meike and Calvert, Daley and Hagedoorn, Jan Marius and Howard, Tom and Klemann, Volker and Lowe, Jason A. and Roberts, Chris and Slangen, Aimee B. A. and Spada, Giorgio},
  title     = {Exploring the drivers of global and local sea-level change over the 21st century and beyond},
  series = {Zweitver{\"o}ffentlichungen der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe},
  journal   = {Zweitver{\"o}ffentlichungen der Universit{\"a}t Potsdam : Mathematisch-Naturwissenschaftliche Reihe},
  number    = {9},
  issn      = {1866-8372},
  doi       = {10.25932/publishup-54988},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-549881},
  pages     = {27},
  year      = {2020},
  abstract  = {We present a new set of global and local sea-level projections at example tide gauge locations under the RCP2.6, RCP4.5, and RCP8.5 emissions scenarios. Compared to the CMIP5-based sea-level projections presented in IPCC AR5, we introduce a number of methodological innovations, including (i) more comprehensive treatment of uncertainties, (ii) direct traceability between global and local projections, and (iii) exploratory extended projections to 2300 based on emulation of individual CMIP5 models. Combining the projections with observed tide gauge records, we explore the contribution to total variance that arises from sea-level variability, different emissions scenarios, and model uncertainty. For the period out to 2300 we further breakdown the model uncertainty by sea-level component and consider the dependence on geographic location, time horizon, and emissions scenario. Our analysis highlights the importance of local variability for sea-level change in the coming decades and the potential value of annual-to-decadal predictions of local sea-level change. Projections to 2300 show a substantial degree of committed sea-level rise under all emissions scenarios considered and highlight the reduced future risk associated with RCP2.6 and RCP4.5 compared to RCP8.5. Tide gauge locations can show large ( > 50\%) departures from the global average, in some cases even reversing the sign of the change. While uncertainty in projections of the future Antarctic ice dynamic response tends to dominate post-2100, we see substantial differences in the breakdown of model variance as a function of location, time scale, and emissions scenario.},
  language  = {en}
}
@article{PalmerGregoryBaggeetal.2020,
  author    = {Palmer, Matthew D. and Gregory, Jonathan and Bagge, Meike and Calvert, Daley and Hagedoorn, Jan Marius and Howard, Tom and Klemann, Volker and Lowe, Jason A. and Roberts, Chris and Slangen, Aimee B. A. and Spada, Giorgio},
  title     = {Exploring the drivers of global and local sea-level change over the 21st century and beyond},
  series = {Earth's future},
  volume    = {8},
  journal   = {Earth's future},
  number    = {9},
  publisher = {Wiley-Blackwell},
  address   = {Hoboken},
  issn      = {2328-4277},
  doi       = {10.1029/2019EF001413},
  pages     = {1 -- 25},
  year      = {2020},
  abstract  = {We present a new set of global and local sea-level projections at example tide gauge locations under the RCP2.6, RCP4.5, and RCP8.5 emissions scenarios. Compared to the CMIP5-based sea-level projections presented in IPCC AR5, we introduce a number of methodological innovations, including (i) more comprehensive treatment of uncertainties, (ii) direct traceability between global and local projections, and (iii) exploratory extended projections to 2300 based on emulation of individual CMIP5 models. Combining the projections with observed tide gauge records, we explore the contribution to total variance that arises from sea-level variability, different emissions scenarios, and model uncertainty. For the period out to 2300 we further breakdown the model uncertainty by sea-level component and consider the dependence on geographic location, time horizon, and emissions scenario. Our analysis highlights the importance of local variability for sea-level change in the coming decades and the potential value of annual-to-decadal predictions of local sea-level change. Projections to 2300 show a substantial degree of committed sea-level rise under all emissions scenarios considered and highlight the reduced future risk associated with RCP2.6 and RCP4.5 compared to RCP8.5. Tide gauge locations can show large ( > 50\%) departures from the global average, in some cases even reversing the sign of the change. While uncertainty in projections of the future Antarctic ice dynamic response tends to dominate post-2100, we see substantial differences in the breakdown of model variance as a function of location, time scale, and emissions scenario.},
  language  = {en}
}