TY - GEN A1 - Lyu, Yu-Xuan A1 - Fu, Qiang A1 - Wilczok, Dominika A1 - Ying, Kejun A1 - King, Aaron A1 - Antebi, Adam A1 - Vojta, Aleksandar A1 - Stolzing, Alexandra A1 - Moskalev, Alexey A1 - Georgievskaya, Anastasia A1 - Maier, Andrea B. A1 - Olsen, Andrea A1 - Groth, Anja A1 - Simon, Anna Katharina A1 - Brunet, Anne A1 - Jamil, Aisyah A1 - Kulaga, Anton A1 - Bhatti, Asif A1 - Yaden, Benjamin A1 - Pedersen, Bente Klarlund A1 - Schumacher, Björn A1 - Djordjevic, Boris A1 - Kennedy, Brian A1 - Chen, Chieh A1 - Huang, Christine Yuan A1 - Correll, Christoph U. A1 - Murphy, Coleen T. A1 - Ewald, Collin Y. A1 - Chen, Danica A1 - Valenzano, Dario Riccardo A1 - Sołdacki, Dariusz A1 - Erritzoe, David A1 - Meyer, David A1 - Sinclair, David A. A1 - Chini, Eduardo Nunes A1 - Teeling, Emma C. A1 - Morgen, Eric A1 - Verdin, Eric A1 - Vernet, Erik A1 - Pinilla, Estefano A1 - Fang, Evandro F. A1 - Bischof, Evelyne A1 - Mercken, Evi M. A1 - Finger, Fabian A1 - Kuipers, Folkert A1 - Pun, Frank W. A1 - Gyülveszi, Gabor A1 - Civiletto, Gabriele A1 - Zmudze, Garri A1 - Blander, Gil A1 - Pincus, Harold A. A1 - McClure, Joshua A1 - Kirkland, James L. A1 - Peyer, James A1 - Justice, Jamie N. A1 - Vijg, Jan A1 - Gruhn, Jennifer R. A1 - McLaughlin, Jerry A1 - Mannick, Joan A1 - Passos, João A1 - Baur, Joseph A. A1 - Betts-LaCroix, Joe A1 - Sedivy, John M. A1 - Speakman, John R. A1 - Shlain, Jordan A1 - Maltzahn, Julia von A1 - Andreasson, Katrin I. A1 - Moody, Kelsey A1 - Palikaras, Konstantinos A1 - Fortney, Kristen A1 - Niedernhofer, Laura J. A1 - Rasmussen, Lene Juel A1 - Veenhoff, Liesbeth M. A1 - Melton, Lisa A1 - Ferrucci, Luigi A1 - Quarta, Marco A1 - Koval, Maria A1 - Marinova, Maria A1 - Hamalainen, Mark A1 - Unfried, Maximilian A1 - Ringel, Michael S. A1 - Filipovic, Milos A1 - Topors, Mourad A1 - Mitin, Natalia A1 - Roy, Nawal A1 - Pintar, Nika A1 - Barzilai, Nir A1 - Binetti, Paolo A1 - Singh, Parminder A1 - Kohlhaas, Paul A1 - Robbins, Paul D. A1 - Rubin, Paul A1 - Fedichev, Peter O. A1 - Kamya, Petrina A1 - Muñoz-Canoves, Pura A1 - de Cabo, Rafael A1 - Faragher, Richard G. A. A1 - Konrad, Rob A1 - Ripa, Roberto A1 - Mansukhani, Robin A1 - Büttner, Sabrina A1 - Wickström, Sara A. A1 - Brunemeier, Sebastian A1 - Jakimov, Sergey A1 - Luo, Shan A1 - Rosenzweig-Lipson, Sharon A1 - Tsai, Shih-Yin A1 - Dimmeler, Stefanie A1 - Rando, Thomas A. A1 - Peterson, Tim R. A1 - Woods, Tina A1 - Wyss-Coray, Tony A1 - Finkel, Toren A1 - Strauss, Tzipora A1 - Gladyshev, Vadim N. A1 - Longo, Valter D. A1 - Dwaraka, Varun B. A1 - Gorbunova, Vera A1 - Acosta-Rodríguez, Victoria A. A1 - Sorrentino, Vincenzo A1 - Sebastiano, Vittorio A1 - Li, Wenbin A1 - Suh, Yousin A1 - Zhavoronkov, Alex A1 - Scheibye-Knudsen, Morten A1 - Bakula, Daniela T1 - Longevity biotechnology: bridging AI, biomarkers, geroscience and clinical applications for healthy longevity T2 - Aging Y1 - 2024 U6 - https://doi.org/10.18632/aging.206135 SN - 1945-4589 VL - 16 IS - 20 SP - 12955 EP - 12976 PB - Impact Journals, LLC ER - TY - GEN A1 - Webber, H. A1 - Cooke, D. A1 - Wang, C. A1 - Asseng, S. A1 - Martre, P. A1 - Ewert, F. A1 - Kimball, B. A1 - Hoogenboom, G. A1 - Evett, S. A1 - Chanzy, A. A1 - Garrigues, S. A1 - Olioso, A. A1 - Copeland, K.S. A1 - Steiner, J.L. A1 - Cammarano, D. A1 - Chen, Y. A1 - Crépeau, M. A1 - Diamantopoulos, E. A1 - Ferrise, R. A1 - Manceau, L. A1 - Gaiser, T. A1 - Gao, Y. A1 - Gayler, S. A1 - Guarin, J.R. A1 - Hunt, T. A1 - Jégo, G. A1 - Padovan, G. A1 - Pattey, E. A1 - Ripoche, D. A1 - Rodríguez, A. A1 - Ruiz-Ramos, M. A1 - Shelia, V. A1 - Srivastava, A.K. A1 - Supit, I. A1 - Tao, F. A1 - Thorp, K. A1 - Viswanathan, M. A1 - Weber, T. A1 - White, J. T1 - Wheat crop models underestimate drought stress in semi-arid and Mediterranean environments T2 - Field crops research N2 - Under climate change and increasingly extreme weather, projections of water demand and drought stress from process-based crop models can inform risk management and adaptation strategies. Previous studies investigating maize crop models demonstrated considerable error in the simulation of water use, and no similar evaluation of wheat crop models exists. The aims of this study were to (1) evaluate wheat crop models’ performance in reproducing observed daily evapotranspiration (ET) for Mediterranean and semi-arid environments, and (2) identify factors and processes associated with model error and uncertainty. These were assessed with an ensemble of wheat crop models for two experiments, one conducted in Bushland, Texas, USA (three seasons, deficit and full irrigation) and another in Avignon, France (four rainfed seasons) with winter bread and durum wheat, respectively. Models were calibrated with all observed data for crop growth. The model ensemble median underestimated water use in all environments evaluated, suggesting a systematic bias. The relative error in underestimating daily ET was constant across levels of atmospheric evaporative demand; therefore, the absolute error was greater for days with larger evaporative demand. This implies errors in the soil water balance increase more rapidly under high evaporative demand conditions. Using a potential versus reference crop evapotranspiration approach did not explain relative model performance. However, the sensitivity analysis indicated that simulation of atmospheric evaporative demand terms explained much more uncertainty in seasonal water use than terms related to soil depth or root growth. Errors in simulated leaf area index were associated with errors in daily simulated ET, but the relationship varied with the growth stage. Collectively, the results suggest the need to improve simulation of atmospheric ET demand to avoid underestimating projected impacts of drought or required water resource availability for viable production systems. KW - Crop models KW - Evapotranspiration KW - Wheat KW - Drought stress KW - Climate risk Y1 - 2025 U6 - https://doi.org/10.1016/j.fcr.2025.110032 SN - 0378-4290 VL - 332 SP - 1 EP - 18 PB - Elsevier BV CY - Amsterdam ER - TY - JOUR A1 - Millán-Rodriguez, J. A1 - Pérez-García, C. A1 - Bestehorn, Michael A1 - Fantz, M. A1 - Friedrich, R. T1 - Pattern Formation in Convection of Rotating Fluids with Broken Vertical Symmetry Y1 - 1992 ER - TY - JOUR A1 - Millán-Rodriguez, J. A1 - Bestehorn, Michael A1 - Pérez-García, C. A1 - Friedrich, R. A1 - Neufeld, M. T1 - Defects Motion in Rotating Fluids Y1 - 1995 ER - TY - JOUR A1 - Millán-Rodriguez, J. A1 - Bestehorn, Michael A1 - Pérez-García, C. A1 - Neufeld, M. A1 - Friedrich, R. T1 - Motion of Defects in Rotating Fluids Y1 - 1994 ER - TY - RPRT A1 - Serrano, J. A1 - Sarmento, H. A1 - Grilo, Antonio A1 - Goncalves, J. A1 - Holczer, T. A1 - Bohli, J. M. A1 - Rodriguez, R. A1 - Garrido, D. A1 - Piotrowski, Krzysztof A1 - Selhorst, M. T1 - Report on System Integration Y1 - 2011 ER - TY - CHAP A1 - Krishnegowda, Karthik A1 - Rodriguez-Vazquez, Pedro A1 - Wolf, Andreas C. A1 - Grzyb, Janusz A1 - Pfeiffer, Ullrich R. A1 - Kraemer, Rolf T1 - 100 Gbps and Beyond: Hardware in the Loop Experiments with PSSS Modulation using 230 GHz Frontend T2 - IEEE 15th Workshop on Positioning, Navigation and Communications (WPNC 2018), Bremen, Germany, 25 - 26 October 2018 Y1 - 2018 SN - 978-1-5386-6436-0 SN - 978-1-5386-6437-7 U6 - https://doi.org/10.1109/WPNC.2018.8555838 PB - IEEE CY - Piscataway ER - TY - GEN A1 - Bissolli, Peter A1 - Demicran, Mesut A1 - Kennedy, John A1 - Lakatos, Mónika A1 - McCarthy, Mark A1 - Morice, Colin A1 - Pastor Saavedra, S. A1 - Pons, M. R. A1 - Rodriguez Camino, C. A1 - Rösner, Benjamin A1 - Sensoy, Serhat A1 - Spillane, Sandra A1 - Trachte, Katja A1 - van der Schrier, Gerard T1 - Europe and the Middle East T2 - Bulletin of the American Meteorological Society / State of the Climate in 2017 N2 - In 2017, the dominant greenhouse gases released into Earth’s atmosphere—carbon dioxide, methane, and nitrous oxide— reached new record highs. The annual global average carbon dioxide concentration at Earth’s surface for 2017 was 405.0 ± 0.1 ppm, 2.2 ppm greater than for 2016 and the highest in the modern atmospheric measurement record and in ice core records dating back as far as 800 000 years. The global growth rate of CO2 has nearly quadrupled since the early 1960s. With ENSO-neutral conditions present in the central and eastern equatorial Pacific Ocean during most of the year and weak La Niña conditions notable at the start and end, the global temperature across land and ocean surfaces ranked as the second or third highest, depending on the dataset, since records began in the mid-to-late 1800s. Notably, it was the warmest non-El Niño year in the instrumental record. Above Earth’s surface, the annual lower tropospheric temperature was also either second or third highest according to all datasets analyzed. The lower stratospheric temperature was about 0.2°C higher than the record cold temperature of 2016 according to most of the in situ and satellite datasets. Several countries, including Argentina, Uruguay, Spain, and Bulgaria, reported record high annual temperatures. Mexico broke its annual record for the fourth consecutive year. On 27 January, the temperature reached 43.4°C at Puerto Madryn, Argentina—the highest temperature recorded so far south (43°S) anywhere in the world. On 28 May in Turbat, western Pakistan, the high of 53.5°C tied Pakistan’s all-time highest temperature and became the world-record highest temperature for May. In the Arctic, the 2017 land surface temperature was 1.6°C above the 1981–2010 average, the second highest since the record began in 1900, behind only 2016. The five highest annual Arctic temperatures have all occurred since 2007. Exceptionally high temperatures were observed in the permafrost across the Arctic, with record values reported in much of Alaska and northwestern Canada. In August, high sea surface temperature (SST) records were broken for the Chukchi Sea, with some regions as warm as +11°C, or 3° to 4°C warmer than the longterm mean (1982–present). According to paleoclimate studies, today’s abnormally warm Arctic air and SSTs have not been observed in the last 2000 years. The increasing temperatures have led to decreasing Arctic sea ice extent and thickness. On 7 March, sea ice extent at the end of the growth season saw its lowest maximum in the 37-year satellite record, covering 8% less area than the 1981–2010 average. The Arctic sea ice minimum on 13 September was the eighth lowest on record and covered 25% less area than the long-term mean. Preliminary data indicate that glaciers across the world lost mass for the 38th consecutive year on record; the declines are remarkably consistent from region to region. Cumulatively since 1980, this loss is equivalent to slicing 22 meters off the top of the average glacier. Antarctic sea ice extent remained below average for all of 2017, with record lows during the first four months. Over the continent, the austral summer seasonal melt extent and melt index were the second highest since 2005, mostly due to strong positive anomalies of air temperature over most of the West Antarctic coast. In contrast, the East Antarctic Plateau saw record low mean temperatures in March. The year was also distinguished by the second smallest Antarctic ozone hole observed since 1988. Across the global oceans, the overall long-term SST warming trend remained strong. Although SST cooled slightly from 2016 to 2017, the last three years produced the three highest annual values observed; these high anomalies have been associated with widespread coral bleaching. The most recent global coral bleaching lasted three full years, June 2014 to May 2017, and was the longest, most widespread, and almost certainly most destructive such event on record. Global integrals of 0–700- m and 0–2000-m ocean heat content reached record highs in 2017, and global mean sea level during the year became the highest annual average in the 25-year satellite altimetry record, rising to 77 mm above the 1993 average. In the tropics, 2017 saw 85 named tropical storms, slightly above the 1981–2010 average of 82. The North Atlantic basin was the only basin that featured an above-normal season, its seventh most active in the 164-year record. Three hurricanes in the basin were especially notable. Harvey produced record rainfall totals in areas of Texas and Louisiana, including a storm total of 1538.7 mm near Beaumont, Texas, which far exceeds the previous known U.S. tropical cyclone record of 1320.8 mm. Irma was the strongest tropical cyclone globally in 2017 and the strongest Atlantic hurricane outside of the Gulf of Mexico and Caribbean on record with maximum winds of 295 km h−1. Maria caused catastrophic destruction across the Caribbean Islands, including devastating wind damage and flooding across Puerto Rico. Elsewhere, the western North Pacific, South Indian, and Australian basins were all particularly quiet. Precipitation over global land areas in 2017 was clearly above the long-term average. Among noteworthy regional precipitation records in 2017, Russia reported its second wettest year on record (after 2013) and Norway experienced its sixth wettest year since records began in 1900. Across India, heavy rain and flood-related incidents during the monsoon season claimed around 800 lives. In August and September, above-normal precipitation triggered the most devastating floods in more than a decade in the Venezuelan states of Bolívar and Delta Amacuro. In Nigeria, heavy rain during August and September caused the Niger and Benue Rivers to overflow, bringing floods that displaced more than 100 000 people. Global fire activity was the lowest since at least 2003; however, high activity occurred in parts of North America, South America, and Europe, with an unusually long season in Spain and Portugal, which had their second and third driest years on record, respectively. Devastating fires impacted British Columbia, destroying 1.2 million hectares of timber, bush, and grassland, due in part to the region’s driest summer on record. In the United States, an extreme western wildfire season burned over 4 million hectares; the total costs of $18 billion tripled the previous U.S. annual wildfire cost record set in 1991. Y1 - 2018 U6 - https://doi.org/10.1175/2018BAMSStateoftheClimate.1 SN - 0003-0007 SN - 1520-0477 VL - 99 IS - 8 SP - 222 EP - 233 ER - TY - GEN A1 - Braud, N. A1 - Wallander, H.J. A1 - Buß, L. A1 - Löfstrand, M. A1 - Blomqvist, J. A1 - Berschauer, C. A1 - Rodriguez, A. Morales A1 - Kofoed, P.M. A1 - Resta, A. A1 - Krisponeit, J.-O. A1 - Schmidt, T. A1 - Lundgren, E. A1 - Flege, J.I. A1 - Falta, J. A1 - Merte, L.R. T1 - Growth, structure, and morphology of ultra-thin tin oxide phases forming on Pt₃Sn(111) single crystals upon exposure to oxygen T2 - Surface science N2 - Here we report an investigation of ultrathin tin oxide films on Pt3Sn(111) using low-energy electron microscopy (LEEM), microspot low-energy electron diffraction (𝜇-LEED), scanning tunneling microscopy (STM), surface X-ray diffraction (SXRD), and high-resolution X-ray photoelectron spectroscopy (XPS). Oxidation at ∼390–410 ◦C produces triangular, two-dimensional oxide islands that nucleate rapidly and exhibit self-limited lateral growth, attributed to limited Sn diffusion from the subsurface of the crystal. 𝜇-LEED shows that the initially formed (4 × 4) Sn oxide is subsequently converted to a more oxygen-rich (2 × 2𝑛) ‘‘stripe’’ phase. At 630 ◦C, enhanced Sn mobility enables a closed (4 × 4) film. The (2 × 2𝑛) phase is shown to consist of a (2 × 2) Sn lattice modulated by 1D stripe defects with spacings of 𝑛 = 4–6 atomic rows; LEED and SXRD measurements show diffraction features corresponding to this striped superstructure. The two oxides can be distinguished in XPS by their O 1s lineshapes: the (4 × 4) phase shows a clear doublet attributable to distinct O species, whereas the (2 × 2𝑛) phase exhibits a broader envelope consistent with a distribution of O coordination environments. The Sn 3d5∕2 spectra are similar for both phases, reflecting closely related Sn bonding motifs. The spectra are consistent with those of previous near-ambient-pressure XPS measurements, suggesting that the surface oxides forming under CO oxidation conditions are similar to those studied here. KW - Tin oxide KW - Platinum-tin KW - LEEM KW - STM KW - SnOx KW - SXRD Y1 - 2026 U6 - https://doi.org/10.1016/j.susc.2025.122927 SN - 0039-6028 SN - 1879-2758 VL - 767 SP - 1 EP - 8 PB - Elsevier BV CY - Amsterdam ER -