Improvement of ubiquitylation site detection by Orbitrap mass spectrometry

Ubiquitylation is an important posttranslational protein modification that is involved in many cellular events. Immunopurification of peptides containing a K-ε-diglycine (diGly) remnant as a mark of ubiquitylation combined with mass spectrometric detection has resulted in an explosion of the number of identified ubiquitylation sites. Here, we present several significant improvements to this workflow, including fast, offline and crude high pH reverse-phase fractionation of tryptic peptides into only three fractions with simultaneous desalting prior to immunopurification and better control of the peptide fragmentation settings in the Orbitrap HCD cell. In addition, more efficient sample cleanup using a filter plug to retain the antibody beads results in a higher specificity for diGly peptides and less non-specific binding. These relatively simple modifications of the protocol result in the routine detection of over 23,000 diGly peptides from HeLa cells upon proteasome inhibition. The efficacy of this strategy is shown for lysates of both non-labeled and SILAC labeled cell lines. Furthermore, we demonstrate that this strategy is useful for the in-depth analysis of the endogenous, unstimulated ubiquitinome of in vivo samples such as mouse brain tissue. This study presents a valuable addition to the toolbox for ubiquitylation site analysis to uncover the deep ubiquitinome. Significance: A K-ε-diglycine (diGly) mark on peptides after tryptic digestion of proteins indicates a site of ubiquitylation, a posttranslational modification involved in a wide range of cellular processes. Here, we report several improvements to methods for the isolation and detection of diGly peptides from complex biological mixtures such as cell lysates and brain tissue. This adapted method is robust, reproducible and outperforms previously published methods in terms of number of modified peptide identifications from a single sample. In-depth analysis of the ubiquitinome using mass spectrometry will lead to a better understanding of the roles of protein ubiquitylation in cellular events

Ice sheet model dependency of the simulated Greenland Ice Sheet in the mid-Pliocene

The understanding of the nature and behavior of ice sheets in past warm periods is important for constraining the potential impacts of future climate change. The Pliocene warm period (between 3.264 and 3.025 Ma) saw global temperatures similar to those projected for future climates; nevertheless, Pliocene ice locations and extents are still poorly constrained. We present results from the efforts to simulate mid-Pliocene Greenland Ice Sheets by means of the international Pliocene Ice Sheet Modeling Intercomparison Project (PLISMIP). We compare the performance of existing numerical ice sheet models in simulating modern control and mid-Pliocene ice sheets with a suite of sensitivity experiments guided by available proxy records. We quantify equilibrated ice sheet volume on Greenland, identifying a potential range in sea level contributions from warm Pliocene scenarios. A series of statistical measures are performed to quantify the confidence of simulations with focus on inter-model and inter-scenario differences. We find that Pliocene Greenland Ice Sheets are less sensitive to differences in ice sheet model configurations and internal physical quantities than to changes in imposed climate forcing. We conclude that Pliocene ice was most likely to be limited to the highest elevations in eastern and southern Greenland as simulated with the highest confidence and by synthesizing available regional proxies; however, the extent of those ice caps needs to be further constrained by using a range of general circulation model (GCM) climate forcings

State of the climate in 2013

In 2013, the vast majority of the monitored climate variables reported here maintained trends established in recent decades. ENSO was in a neutral state during the entire year, remaining mostly on the cool side of neutral with modest impacts on regional weather patterns around the world. This follows several years dominated by the effects of either La Niña or El Niño events. According to several independent analyses, 2013 was again among the 10 warmest years on record at the global scale, both at the Earths surface and through the troposphere. Some regions in the Southern Hemisphere had record or near-record high temperatures for the year. Australia observed its hottest year on record, while Argentina and New Zealand reported their second and third hottest years, respectively. In Antarctica, Amundsen-Scott South Pole Station reported its highest annual temperature since records began in 1957. At the opposite pole, the Arctic observed its seventh warmest year since records began in the early 20th century. At 20-m depth, record high temperatures were measured at some permafrost stations on the North Slope of Alaska and in the Brooks Range. In the Northern Hemisphere extratropics, anomalous meridional atmospheric circulation occurred throughout much of the year, leading to marked regional extremes of both temperature and precipitation. Cold temperature anomalies during winter across Eurasia were followed by warm spring temperature anomalies, which were linked to a new record low Eurasian snow cover extent in May. Minimum sea ice extent in the Arctic was the sixth lowest since satellite observations began in 1979. Including 2013, all seven lowest extents on record have occurred in the past seven years. Antarctica, on the other hand, had above-average sea ice extent throughout 2013, with 116 days of new daily high extent records, including a new daily maximum sea ice area of 19.57 million km2 reached on 1 October. ENSO-neutral conditions in the eastern central Pacific Ocean and a negative Pacific decadal oscillation pattern in the North Pacific had the largest impacts on the global sea surface temperature in 2013. The North Pacific reached a historic high temperature in 2013 and on balance the globally-averaged sea surface temperature was among the 10 highest on record. Overall, the salt content in nearsurface ocean waters increased while in intermediate waters it decreased. Global mean sea level continued to rise during 2013, on pace with a trend of 3.2 mm yr-1 over the past two decades. A portion of this trend (0.5 mm yr-1) has been attributed to natural variability associated with the Pacific decadal oscillation as well as to ongoing contributions from the melting of glaciers and ice sheets and ocean warming. Global tropical cyclone frequency during 2013 was slightly above average with a total of 94 storms, although the North Atlantic Basin had its quietest hurricane season since 1994. In the Western North Pacific Basin, Super Typhoon Haiyan, the deadliest tropical cyclone of 2013, had 1-minute sustained winds estimated to be 170 kt (87.5 m s-1) on 7 November, the highest wind speed ever assigned to a tropical cyclone. High storm surge was also associated with Haiyan as it made landfall over the central Philippines, an area where sea level is currently at historic highs, increasing by 200 mm since 1970. In the atmosphere, carbon dioxide, methane, and nitrous oxide all continued to increase in 2013. As in previous years, each of these major greenhouse gases once again reached historic high concentrations. In the Arctic, carbon dioxide and methane increased at the same rate as the global increase. These increases are likely due to export from lower latitudes rather than a consequence of increases in Arctic sources, such as thawing permafrost. At Mauna Loa, Hawaii, for the first time since measurements began in 1958, the daily average mixing ratio of carbon dioxide exceeded 400 ppm on 9 May. The state of these variables, along with dozens of others, and the 2013 climate conditions of regions around the world are discussed in further detail in this 24th edition of the State of the Climate series. © 2014, American Meteorological Society. All rights reserved

The lumping of heat transfer parameters in cooled packed beds: effect of the bed entry

The lumping of the heat transfer parameters of the one- and the two-dimensional pseudo-homogeneous model of a cooled fixed bed were compared. It appeared that the lumping of the two-dimensional parameters, being the effective radial conductivity h-eff and the heat transfer coefficient at the wall (alpha)w, into the one-dimensional overall heat transfer coefficient U results in a length dependence of U. It is shown that the ratio (alpha)w/U develops from unity at the bed inlet to a final value. The magnitude of this final value depends on the Biot number, whereas the length of this transition section is affected by the Peclet number. A new relation to lump the effective conductivity and the heat transfer coefficient at the wall into an overall heat transfer coefficient which depends on the values of the Biot number and the Peclet number is presented. This relation accounts for both the magnitude and the transition length of the ratio (alpha)w/U