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科学家首次证实地球氧同位素比率取决于地球内部热流 快报文章
地球科学快报,2023年第1期
作者:  张树良
Microsoft Word(14Kb)  |  收藏  |  浏览/下载:582/0  |  提交时间:2023/01/10
oxygen isotope ratios  Earth's thermal evolution  heat flow  sedimentary rock  chert  
气候介导的温度波动变化促进物种灭绝风险 快报文章
气候变化快报,2022年第21期
作者:  刘莉娜
Microsoft Word(13Kb)  |  收藏  |  浏览/下载:664/1  |  提交时间:2022/11/04
Temperature fluctuations  Climate change  Extinction  Thermal stress  
研究表明地球内部冷却速度快于预期 快报文章
地球科学快报,2022年第03期
作者:  王晓晨
Microsoft Word(16Kb)  |  收藏  |  浏览/下载:672/0  |  提交时间:2022/02/10
Radiative thermal conductivity  core-mantle boundary  
气候变化驱动湖泊热栖息地变化 快报文章
资源环境快报,2021年第11期
作者:  吴秀平
Microsoft Word(13Kb)  |  收藏  |  浏览/下载:400/0  |  提交时间:2021/06/17
Climate change  lake thermal habitat  
The Orinoco Low-Level Jet: An Investigation of Its Mechanisms of Formation Using the WRF Model 期刊论文
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2020, 125 (13)
作者:  Jimenez-Sanchez, Giovanni;  Markowski, Paul M.;  Young, George S.;  Stensrud, David J.
收藏  |  浏览/下载:11/0  |  提交时间:2020/08/18
Orinoco low-level jet  forcing mechanisms  dynamical downscaling  momentum balance analysis  LLJs near the equator may originate from processes other than the inertial oscillation  LLJs near the equator may originate from processes other than topographic thermal forcing  
A remnant planetary core in the hot-Neptune desert 期刊论文
NATURE, 2020, 583 (7814) : 39-+
作者:  David J. Armstrong;  Thé;  o A. Lopez;  Vardan Adibekyan;  Richard A. Booth;  Edward M. Bryant;  Karen A. Collins;  Magali Deleuil;  Alexandre Emsenhuber;  Chelsea X. Huang;  George W. King;  Jorge Lillo-Box;  Jack J. Lissauer;  Elisabeth Matthews;  Olivier Mousis;  Louise D. Nielsen;  Hugh Osborn;  Jon Otegi;  Nuno C. Santos;  ;  rgio G. Sousa;  Keivan G. Stassun;  Dimitri Veras;  Carl Ziegler;  Jack S. Acton;  Jose M. Almenara;  David R. Anderson;  David Barrado;  Susana C. C. Barros;  Daniel Bayliss;  Claudia Belardi;  Francois Bouchy;  ;  sar Briceñ;  o;  Matteo Brogi;  David J. A. Brown;  Matthew R. Burleigh;  Sarah L. Casewell;  Alexander Chaushev;  David R. Ciardi;  Kevin I. Collins;  Knicole D. Coló;  n;  Benjamin F. Cooke;  Ian J. M. Crossfield;  Rodrigo F. Dí;  az;  Elisa Delgado Mena;  Olivier D. S. Demangeon;  Caroline Dorn;  Xavier Dumusque;  Philipp Eigmü;  ller;  Michael Fausnaugh;  Pedro Figueira;  Tianjun Gan;  Siddharth Gandhi;  Samuel Gill;  Erica J. Gonzales;  Michael R. Goad;  Maximilian N. Gü;  nther;  Ravit Helled;  Saeed Hojjatpanah;  Steve B. Howell;  James Jackman;  James S. Jenkins;  Jon M. Jenkins;  Eric L. N. Jensen;  Grant M. Kennedy;  David W. Latham;  Nicholas Law;  Monika Lendl;  Michael Lozovsky;  Andrew W. Mann;  Maximiliano Moyano;  James McCormac;  Farzana Meru;  Christoph Mordasini;  Ares Osborn;  Don Pollacco;  Didier Queloz;  Liam Raynard;  George R. Ricker;  Pamela Rowden;  Alexandre Santerne;  Joshua E. Schlieder;  Sara Seager;  Lizhou Sha;  Thiam-Guan Tan;  Rosanna H. Tilbrook;  Eric Ting;  Sté;  phane Udry;  Roland Vanderspek;  Christopher A. Watson;  Richard G. West;  Paul A. Wilson;  Joshua N. Winn;  Peter Wheatley;  Jesus Noel Villasenor;  Jose I. Vines;  Zhuchang Zhan
收藏  |  浏览/下载:17/0  |  提交时间:2020/07/06

The interiors of giant planets remain poorly understood. Even for the planets in the Solar System, difficulties in observation lead to large uncertainties in the properties of planetary cores. Exoplanets that have undergone rare evolutionary processes provide a route to understanding planetary interiors. Planets found in and near the typically barren hot-Neptune '  desert'  (1,2)(a region in mass-radius space that contains few planets) have proved to be particularly valuable in this regard. These planets include HD149026b(3), which is thought to have an unusually massive core, and recent discoveries such as LTT9779b(4)and NGTS-4b(5), on which photoevaporation has removed a substantial part of their outer atmospheres. Here we report observations of the planet TOI-849b, which has a radius smaller than Neptune'  s but an anomalously large mass of39.1-2.6+2.7Earth masses and a density of5.2-0.8+0.7grams per cubic centimetre, similar to Earth'  s. Interior-structure models suggest that any gaseous envelope of pure hydrogen and helium consists of no more than3.9-0.9+0.8 per cent of the total planetary mass. The planet could have been a gas giant before undergoing extreme mass loss via thermal self-disruption or giant planet collisions, or it could have avoided substantial gas accretion, perhaps through gap opening or late formation(6). Although photoevaporation rates cannot account for the mass loss required to reduce a Jupiter-like gas giant, they can remove a small (a few Earth masses) hydrogen and helium envelope on timescales of several billion years, implying that any remaining atmosphere on TOI-849b is likely to be enriched by water or other volatiles from the planetary interior. We conclude that TOI-849b is the remnant core of a giant planet.


Observations of TOI-849b reveal a radius smaller than Neptune'  s but a large mass of about 40 Earth masses, indicating that the planet is the remnant core of a gas giant.


  
热带森林的固碳作用存在温度临界点 快报文章
气候变化快报,2020年第12期
作者:  裴惠娟
Microsoft Word(15Kb)  |  收藏  |  浏览/下载:416/0  |  提交时间:2020/06/19
Tropical Forests  Thermal Sensitivity  
A population of dust-enshrouded objects orbiting the Galactic black hole 期刊论文
NATURE, 2020, 577 (7790) : 337-+
作者:  Witze, Alexandra
收藏  |  浏览/下载:8/0  |  提交时间:2020/07/03

The central 0.1 parsecs of the Milky Way host a supermassive black hole identified with the position of the radio and infrared source Sagittarius A* (refs.(1,2)), a cluster of young, massive stars (the S stars3) and various gaseous features(4,5). Recently, two unusual objects have been found to be closely orbiting Sagittarius A*: the so-called G sources, G1 and G2. These objects are unresolved (having a size of the order of 100 astronomical units, except at periapse, where the tidal interaction with the black hole stretches them along the orbit) and they show both thermal dust emission and line emission from ionized gas(6-10). G1 and G2 have generated attention because they appear to be tidally interacting with the supermassive Galactic black hole, possibly enhancing its accretion activity. No broad consensus has yet been reached concerning their nature: the G objects show the characteristics of gas and dust clouds but display the dynamical properties of stellar-mass objects. Here we report observations of four additional G objects, all lying within 0.04 parsecs of the black hole and forming a class that is probably unique to this environment. The widely varying orbits derived for the six G objects demonstrate that they were commonly but separately formed.


  
The Insulating Effect of Methane Clathrate Crust on Titan's Thermal Evolution 期刊论文
GEOPHYSICAL RESEARCH LETTERS, 2020, 47 (13)
作者:  Kalousova, Klara;  Sotin, Christophe
收藏  |  浏览/下载:10/0  |  提交时间:2020/06/16
Titan  clathrates  thermal evolution  ocean  
Solar reflective pavements-A policy panacea to heat mitigation? 期刊论文
ENVIRONMENTAL RESEARCH LETTERS, 2020, 15 (6)
作者:  Middel, Ariane;  Turner, V. Kelly;  Schneider, Florian A.;  Zhang, Yujia;  Stiller, Matthew
收藏  |  浏览/下载:8/0  |  提交时间:2020/08/18
cool pavement  urban heat island  heat mitigation  pedestrian thermal exposure