Author Correction: Global glacier mass changes and their contributions to sea-level rise from 1961 to 2016.

An Amendment to this paper has been published and can be accessed via a link at the top of the paper.

Global glacier mass changes and their contributions to sea-level rise from 1961 to 2016.

Glaciers distinct from the Greenland and Antarctic ice sheets cover an area of approximately 706,000 square kilometres globally1, with an estimated total volume of 170,000 cubic kilometres, or 0.4 metres of potential sea-level-rise equivalent2. Retreating and thinning glaciers are icons of climate change3 and affect regional runoff4 as well as global sea level5,6. In past reports from the Intergovernmental Panel on Climate Change, estimates of changes in glacier mass were based on the multiplication of averaged or interpolated results from available observations of a few hundred glaciers by defined regional glacier areas7-10. For data-scarce regions, these results had to be complemented with estimates based on satellite altimetry and gravimetry11. These past approaches were challenged by the small number and heterogeneous spatiotemporal distribution of in situ measurement series and their often unknown ability to represent their respective mountain ranges, as well as by the spatial limitations of satellite altimetry (for which only point data are available) and gravimetry (with its coarse resolution). Here we use an extrapolation of glaciological and geodetic observations to show that glaciers contributed 27 ± 22 millimetres to global mean sea-level rise from 1961 to 2016. Regional specific-mass-change rates for 2006-2016 range from -0.1 metres to -1.2 metres of water equivalent per year, resulting in a global sea-level contribution of 335 ± 144 gigatonnes, or 0.92 ± 0.39 millimetres, per year. Although statistical uncertainty ranges overlap, our conclusions suggest that glacier mass loss may be larger than previously reported11. The present glacier mass loss is equivalent to the sea-level contribution of the Greenland Ice Sheet12, clearly exceeds the loss from the Antarctic Ice Sheet13, and accounts for 25 to 30 per cent of the total observed sea-level rise14. Present mass-loss rates indicate that glaciers could almost disappear in some mountain ranges in this century, while heavily glacierized regions will continue to contribute to sea-level rise beyond 2100.

[Breast pain and fever in a 46-year-old immunosuppressed patient with breast implants]. / Schmerzen im Bereich der Mamma und Fieber bei einer 46­Jährigen mit Immunsuppression und Mammaaugmentation.

A 46-year-old immunosuppressed patient presented with a breast implant-associated infection 10 years after breast augmentation in Southeast Asia. No pathogen was identified in the initial conventional microbiological workup. Subsequently, infection with Mycobacterium abscessus-a nontuberculous mycobacteria-was diagnosed using a special culture technique. Increased rates of such infections are reported after cosmetic surgery in foreign countries, presumably due to inoculation with these ubiquitous pathogens. This case highlights the fact that the differential diagnosis and thus the microbiological workup should be extended in cases without initial pathogen detection.

Standardization of oncoplastic breast conserving surgery.

The emphasis on esthetic outcomes and quality of life after breast cancer surgery has motivated surgeons to develop oncoplastic breast conserving surgery (OPS). Training programs are still rare in most countries, and there is little standardization, which challenges the scientific evaluation of the techniques. The present article attempts to standardize OPS nomenclature, indications, and reconstruction choice selection embedded in a thorough review of the literature. We propose four breast conserving surgery (BCS) categories: Conventional tumorectomy, oncoplastic mastopexy, oncoplastic tumorectomy and oncoplastic reduction mammoplasty. The main volume displacement techniques are glandular re-approximation, use of tailored glandular or dermoglandular flaps and nipple-areola complex pedicles. We developed an indication algorithm based on the size and shape of the breast as well as the size and location of the tumor. A reconstruction algorithm suggests a selection of suitable tailored flaps and pedicles based on tumor location and vascular supply of the breast. The application of these algorithms results in known and novel OPS techniques, which are presented here with long-term results. We designed the algorithms to help tailor every operation to the individual patient in a standardized manner, since OPS is now on the rise, more than two decades after the publication of the first techniques. A rapidly increasing body of observational evidence suggests comparable rates of local recurrence between OPS and conventional BCS. Importantly, the rates of clear resection margins are in favor of OPS despite extended indications to larger tumors. Finally, OPS optimizes patient satisfaction by improving esthetic outcomes after BCS.