supported by the National Natural Science Foundation of China(42250101);the Macao Foundation and China National Space Administration。
The scientific research of geomagnetism has been largely driven by new geomagnetic data that are available to scientists.Macao Science Satellite-1(MSS-1)was successfully launched on 21st May 2023 into a near-circular ...
supported by the Macao Foundation and preresearch project on Civil Aerospace Technologies of CNSA(D020308,D020303);the Macao Science and Technology Development Fund(0001/2019/A1);the National Natural Science Foundation of China(41904066,42142034)。
Earth’s magnetic field is generated in the fluid outer core through the dynamo process.Over the last decade,data assimilation has been used to retrieve the core dynamics and predict the evolution of the geomagnetic f...
supported by Macao Science and Technology Development Fund grant 0001/2019/A1;Macao Foundation;the preresearch Project on Civil Aerospace Technologies of CNSA(Grants No.D020303 and D020308);the National Natural Science Foundation of China(41904066,42142034)。
Earth’s magnetic field,which is generated in the liquid outer core through the dynamo action,undergoes changes on timescales of a few years to several million years,yet the underlying mechanisms responsible for the f...
financial support from the National Natural Science Foundation of China(Grant Nos.41804082 and 41873073);the Special Research Assistant Funding Program provided by the Chinese Academy of Sciences。
The Earth’s core is composed of iron,nickel,and a small amount of light elements(e.g.,Si,S,O,C,N,H and P).The thermal conductivities of these components dominate the adiabatic heat flow in the core,which is highly co...
Ministry of Earth Sciences,Government of India for financial support under the project grant no.MoES/16/25/10-RDEAS;DST,INSPIRE program by Department of Science and Technology,Government of India for financial support。
Thermal conductivity(k)of iron is measured up to about 134 GPa.The measurements are carried out using the single sided laser heated diamond anvil cell,where the power absorbed by a Fe metal foil at hotspot is calculat...
With the support by the National Natural Science Foundation of China and the Chinese Academy of Sciences,the research team led by Prof.Wei Yong(魏勇)at the Key Laboratory of Earth and Planetary Physics,Institute of Ge...
supported by NASA Earth Surface and Interior (ESI) Program (W.K.and J.C.);NASA Geomagnetic Infrastructure Fund;NASA GSFC SEEC Fund (W.K.);NASA GRACE Project (J.C.);Taiwan Ministry of Science and Technology via grant 106-2116-M-001-013(B. F. Chao);NASA GSFC fellowship program;IES of Academia Sinica for support of visiting tenure
The observed Earth’s polar motion on decadal time scales has long been conjectured to be excited by the exchange of equatorial angular momentum between the solid mantle and the fluid outer core,via the mechanism of e...
It is commonly known that the climate debate suffers due to a lack of knowledge about the cause and effect relationship between a number of climatic temperature variations that have occurred in history without being a...
supported by the National Science Foundation of USA(Nos.EAR 07-38492 and EAR 11-60917)
Seismic P velocity structure is determined for the upper 500 km of the inner core and lowermost 200 km of the outer core from differential travel times and amplitude ratios. Results confirm the existence of a globally...
This research is supported by NSF Mathematical Geosciences program under the grants EAR-0327875 and EAR-0327843,NASA Solid Earth and Natural Hazard Program,NASA Mars Fundamental Research Program.We also thank GSFC NPPCS and NASA NAS for computation support.
Constraining numerical geodynamo models with surface geomagnetic observationsis very important in many respects:it directly helps to improve numericalgeodynamo models,and expands their geophysical applications beyond ...