| 1. |
- Ades, M., et al.
(författare)
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Global Climate : in State of the climate in 2019
- 2020
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Ingår i: Bulletin of The American Meteorological Society - (BAMS). - : American Meteorological Society. - 0003-0007 .- 1520-0477. ; 101:8, s. S17-S127
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Tidskriftsartikel (refereegranskat)
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| 2. |
- Ades, M., et al.
(författare)
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GLOBAL CLIMATE
- 2020
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Ingår i: BULLETIN OF THE AMERICAN METEOROLOGICAL SOCIETY. - 0003-0007 .- 1520-0477. ; 101:8
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Tidskriftsartikel (refereegranskat)
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| 3. |
- Cremer, Roxana, 1993-, et al.
(författare)
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Investigating the role of air mass history on the diversity of GCMestimates of atmospheric black carbon in the Arctic
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Annan publikation (övrigt vetenskapligt/konstnärligt)abstract
- Black Carbon (BC) aerosols are known to play an important role in the Arctic, yet their exact contribution to thechanging of the Earth’s climate and Arctic amplification remains unclear. To reduce these uncertainties, the life cycle of BCneeds to be accurately described in general circulation models (GCMs). In this study, four GCMs (ECHAM6.3-HAM2.3,ECHAM6.3-HAM2.3-P3, ECHAM6.3-HAM2.3-SALSA2 and UKESM1.0) are compared in terms of their representation ofBC in the Arctic. A new Lagrangian framework is applied to investigate the history of airmasses reaching the Arctic observationalsite Zeppelin on Svalbard, and compared to the corresponding transport simulated by the GCMs, which are allnudged to reanalysis data from ERA-Interim. Aerosol processes along the trajectories are then compared between the models.ECHAM6.3-HAM2.3-P3 simulates the highest and UKESM1.0 the lowest BC loadings both globally and within the Arcticand ECHAM6.3-HAM2.3-SALSA2 is the GCM that reproduces the observations from Zeppelin station most faithfully. The BC concentration in the Arctic is largely controlled by the wet removal processes described in the models, but dry depositionalso plays a role in explaining some of the inter-model diversity. ECHAM6.3-HAM2.3-P3 is less efficient in wet removal thanthe other models, which is likely a result of an adjusted representation of ice processes compared with the other two ECHAMvariants. UKESM1.0 is the most efficient model in removing BC from the atmosphere, in large part due to more efficient dryremoval than with the ECHAM models. The Lagrangian analysis reveals that the BC concentrations at the Zeppelin station are largely determined by concentrations in airmasses older than the length of our back trajectories, i.e. ten days, highlighting theimportance of remote emissions to local BC concentrations in the Arctic. This further suggests a longer BC lifetime within theArctic as compared with the global average. Our results underline the importance of accurate descriptions of cloud and precipitation microphysics, along with realistic dry and wet scavenging schemes for improved descriptions of BC and its climateimpacts in the Arctic within GCMs.
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| 4. |
- de Miranda, Noel F. C. C., et al.
(författare)
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DNA repair genes are selectively mutated in diffuse large B cell lymphomas
- 2013
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Ingår i: Journal of Experimental Medicine. - : Rockefeller University Press. - 0022-1007 .- 1540-9538. ; 210:9, s. 1729-1742
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Tidskriftsartikel (refereegranskat)abstract
- DNA repair mechanisms are fundamental for B cell development, which relies on the somatic diversification of the immunoglobulin genes by V(D)J recombination, somatic hypermutation, and class switch recombination. Their failure is postulated to promote genomic instability and malignant transformation in B cells. By performing targeted sequencing of 73 key DNA repair genes in 29 B cell lymphoma samples, somatic and germline mutations were identified in various DNA repair pathways, mainly in diffuse large B cell lymphomas (DLBCLs). Mutations in mismatch repair genes (EXO1, MSH2, and MSH6) were associated with microsatellite instability, increased number of somatic insertions/deletions, and altered mutation signatures in tumors. Somatic mutations in nonhomologous end-joining (NHEJ) genes (DCLRE1C/ARTEMIS, PRKDC/DNA-PKcs, XRCC5/KU80, and XRCC6/KU70) were identified in four DLBCL tumors and cytogenetic analyses revealed that translocations involving the immunoglobulin-heavy chain locus occurred exclusively in NHEJ-mutated samples. The novel mutation targets, CHEK2 and PARP1, were further screened in expanded DLBCL cohorts, and somatic as well as novel and rare germline mutations were identified in 8 and 5% of analyzed tumors, respectively. By correlating defects in a subset of DNA damage response and repair genes with genomic instability events in tumors, we propose that these genes play a role in DLBCL lymphomagenesis.
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| 5. |
- Ghan, Steven, et al.
(författare)
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Challenges in constraining anthropogenic aerosol effects on cloud radiative forcing using present-day spatiotemporal variability
- 2016
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Ingår i: Proceedings of the National Academy of Sciences of the United States of America. - : Proceedings of the National Academy of Sciences. - 0027-8424 .- 1091-6490. ; 113:21, s. 5804-5811
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Tidskriftsartikel (refereegranskat)abstract
- A large number of processes are involved in the chain from emissions of aerosol precursor gases and primary particles to impacts on cloud radiative forcing. Those processes are manifest in a number of relationships that can be expressed as factors dlnX/dlnY driving aerosol effects on cloud radiative forcing. These factors include the relationships between cloud condensation nuclei (CCN) concentration and emissions, droplet number and CCN concentration, cloud fraction and droplet number, cloud optical depth and droplet number, and cloud radiative forcing and cloud optical depth. The relationship between cloud optical depth and droplet number can be further decomposed into the sum of two terms involving the relationship of droplet effective radius and cloud liquid water path with droplet number. These relationships can be constrained using observations of recent spatial and temporal variability of these quantities. However, we are most interested in the radiative forcing since the preindustrial era. Because few relevant measurements are available from that era, relationships from recent variability have been assumed to be applicable to the preindustrial to present-day change. Our analysis of Aerosol Comparisons between Observations and Models (AeroCom) model simulations suggests that estimates of relationships from recent variability are poor constraints on relationships from anthropogenic change for some terms, with even the sign of some relationships differing in many regions. Proxies connecting recent spatial/temporal variability to anthropogenic change, or sustained measurements in regions where emissions have changed, are needed to constrain estimates of anthropogenic aerosol impacts on cloud radiative forcing.
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| 6. |
- Gibson, Kate L, et al.
(författare)
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B-cell diversity decreases in old age and is correlated with poor health status
- 2009
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Ingår i: AGING CELL. - : Wiley. - 1474-9718 .- 1474-9726. ; 8:1, s. 18-25
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Tidskriftsartikel (refereegranskat)abstract
- Older people suffer from a decline in immune system, which affects their ability to respond to infections and to raise efficient responses to vaccines. Effective and specific antibodies in responses from older individuals are decreased in favour of non-specific antibody production. We investigated the B-cell repertoire in DNA samples from peripheral blood of individuals aged 86-94 years, and a control group aged 19-54 years, using spectratype analysis of the IGHV complementarity determining region (CDR)3. We found that a proportion of older individuals had a dramatic collapse in their B-cell repertoire diversity. Sequencing of polymerase chain reaction products from a selection of samples indicated that this loss of diversity was characterized by clonal expansions of B cells in vivo. Statistical analysis of the spectratypes enabled objective comparisons and showed that loss of diversity correlated very strongly with the general health status of the individuals; a distorted spectratype can be used to predict frailty. Correlations with survival and vitamin B12 status were also seen. We conclude that B-cell diversity can decrease dramatically with age and may have important implications for the immune health of older people. B-cell immune frailty is also a marker of general frailty.
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| 7. |
- Zhang, Shipeng, et al.
(författare)
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On the characteristics of aerosol indirect effect based on dynamic regimes in global climate models
- 2016
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Ingår i: Atmospheric Chemistry And Physics. - : Copernicus GmbH. - 1680-7316 .- 1680-7324. ; 16:5, s. 2765-2783
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Tidskriftsartikel (refereegranskat)abstract
- Aerosol-cloud interactions continue to constitute a major source of uncertainty for the estimate of climate radiative forcing. The variation of aerosol indirect effects (AIE) in climate models is investigated across different dynamical regimes, determined by monthly mean 500 hPa vertical pressure velocity (omega(500)), lower-tropospheric stability (LTS) and large-scale surface precipitation rate derived from several global climate models (GCMs), with a focus on liquid water path (LWP) response to cloud condensation nuclei (CCN) concentrations. The LWP sensitivity to aerosol perturbation within dynamic regimes is found to exhibit a large spread among these GCMs. It is in regimes of strong large-scale ascent (omega(500)aEuro-aEuro parts per thousand < aEuro-a'25 hPa day(-1)) and low clouds (stratocumulus and trade wind cumulus) where the models differ most. Shortwave aerosol indirect forcing is also found to differ significantly among different regimes. Shortwave aerosol indirect forcing in ascending regimes is close to that in subsidence regimes, which indicates that regimes with strong large-scale ascent are as important as stratocumulus regimes in studying AIE. It is further shown that shortwave aerosol indirect forcing over regions with high monthly large-scale surface precipitation rate (> 0.1 mm day(-1)) contributes the most to the total aerosol indirect forcing (from 64 to nearly 100 %). Results show that the uncertainty in AIE is even larger within specific dynamical regimes compared to the uncertainty in its global mean values, pointing to the need to reduce the uncertainty in AIE in different dynamical regimes.
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