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Nature

Resumen/Descripción – provisto por la editorial en inglés
Nature is a weekly international journal publishing the finest peer-reviewed research in all fields of science and technology on the basis of its originality, importance, interdisciplinary interest, timeliness, accessibility, elegance and surprising conclusions. Nature also provides rapid, authoritative, insightful and arresting news and interpretation of topical and coming trends affecting science, scientists and the wider public.
Palabras clave – provistas por la editorial

No disponibles.

Disponibilidad
Institución detectada Período Navegá Descargá Solicitá
No detectada desde jul. 2012 / hasta dic. 2023 Nature.com
No detectada desde jul. 2006 / hasta ago. 2012 Ovid

Información

Tipo de recurso:

revistas

ISSN impreso

0028-0836

ISSN electrónico

1476-4687

Editor responsable

Springer Nature

País de edición

Reino Unido

Fecha de publicación

Tabla de contenidos

FDA to require diversity plan for clinical trials

Max Kozlov

Palabras clave: Multidisciplinary.

Pp. No disponible

Brain and behaviour: understanding the neural effects of cannabis

Dom Byrne

Palabras clave: Multidisciplinary.

Pp. No disponible

Genome editor tackles disease that can cause sudden death

Palabras clave: Multidisciplinary.

Pp. No disponible

Controlled growth of perovskite layers with volatile alkylammonium chlorides

Jaewang Park; Jongbeom Kim; Hyun-Sung Yun; Min Jae Paik; Eunseo Noh; Hyun Jung Mun; Min Gyu KimORCID; Tae Joo ShinORCID; Sang Il SeokORCID

Palabras clave: Multidisciplinary.

Pp. No disponible

The case for standardizing gene nomenclature in vertebrates

Fiona M. McCarthyORCID; Tamsin E. M. Jones; Anne E. KwitekORCID; Cynthia L. SmithORCID; Peter D. VizeORCID; Monte WesterfieldORCID; Elspeth A. BrufordORCID

Palabras clave: Multidisciplinary.

Pp. E31-E32

High variability reveals complexity under Thwaites Glacier

Craig McConnochieORCID

Palabras clave: Multidisciplinary.

Pp. 420-422

A universal interface for plug-and-play assembly of stretchable devices

Ying JiangORCID; Shaobo JiORCID; Jing Sun; Jianping Huang; Yuanheng LiORCID; Guijin ZouORCID; Teddy SalimORCID; Changxian Wang; Wenlong LiORCID; Haoran JinORCID; Jie XuORCID; Sihong Wang; Ting LeiORCID; Xuzhou YanORCID; Wendy Yen Xian Peh; Shih-Cheng YenORCID; Zhihua LiuORCID; Mei Yu; Hang Zhao; Zechao Lu; Guanglin Li; Huajian GaoORCID; Zhiyuan LiuORCID; Zhenan BaoORCID; Xiaodong ChenORCID

Palabras clave: Multidisciplinary.

Pp. 456-462

Suppressed basal melting in the eastern Thwaites Glacier grounding zone

Peter E. D. DavisORCID; Keith W. NichollsORCID; David M. HollandORCID; Britney E. Schmidt; Peter Washam; Kiya L. Riverman; Robert J. Arthern; Irena VaňkováORCID; Clare EayrsORCID; James A. SmithORCID; Paul G. D. Anker; Andrew D. MullenORCID; Daniel DichekORCID; Justin D. Lawrence; Matthew M. Meister; Elisabeth Clyne; Aurora Basinski-Ferris; Eric RignotORCID; Bastien Y. QuesteORCID; Lars BoehmeORCID; Karen J. HeywoodORCID; Sridhar Anandakrishnan; Keith Makinson

<jats:title>Abstract</jats:title><jats:p>Thwaites Glacier is one of the fastest-changing ice–ocean systems in Antarctica<jats:sup>1–3</jats:sup>. Much of the ice sheet within the catchment of Thwaites Glacier is grounded below sea level on bedrock that deepens inland<jats:sup>4</jats:sup>, making it susceptible to rapid and irreversible ice loss that could raise the global sea level by more than half a metre<jats:sup>2,3,5</jats:sup>. The rate and extent of ice loss, and whether it proceeds irreversibly, are set by the ocean conditions and basal melting within the grounding-zone region where Thwaites Glacier first goes afloat<jats:sup>3,6</jats:sup>, both of which are largely unknown. Here we show—using observations from a hot-water-drilled access hole—that the grounding zone of Thwaites Eastern Ice Shelf (TEIS) is characterized by a warm and highly stable water column with temperatures substantially higher than the in situ freezing point. Despite these warm conditions, low current speeds and strong density stratification in the ice–ocean boundary layer actively restrict the vertical mixing of heat towards the ice base<jats:sup>7,8</jats:sup>, resulting in strongly suppressed basal melting. Our results demonstrate that the canonical model of ice-shelf basal melting used to generate sea-level projections cannot reproduce observed melt rates beneath this critically important glacier, and that rapid and possibly unstable grounding-line retreat may be associated with relatively modest basal melt rates.</jats:p>

Palabras clave: Multidisciplinary.

Pp. 479-485

Was famed poet Pablo Neruda poisoned? Scientists warn case not closed

Michele Catanzaro

Palabras clave: Multidisciplinary.

Pp. No disponible

Towards quantum computers that are robust to errors

Palabras clave: Multidisciplinary.

Pp. No disponible