Lulu Jia

ORCID: 0009-0007-0160-9394
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About
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Research Areas
  • Geophysics and Gravity Measurements
  • GNSS positioning and interference
  • Geomagnetism and Paleomagnetism Studies
  • Cryospheric studies and observations
  • Geological and Geophysical Studies
  • Solar and Space Plasma Dynamics
  • earthquake and tectonic studies
  • Inertial Sensor and Navigation
  • High-pressure geophysics and materials
  • Computational Physics and Python Applications
  • Environmental and Agricultural Sciences
  • Scientific Research and Discoveries
  • Arctic and Antarctic ice dynamics
  • Geophysical and Geoelectrical Methods
  • Geology and Paleoclimatology Research
  • Climate change and permafrost
  • Automated Road and Building Extraction
  • Earthquake Detection and Analysis
  • Remote Sensing and Land Use
  • Groundwater and Isotope Geochemistry
  • Bacteriophages and microbial interactions
  • RNA Interference and Gene Delivery
  • Geological and Geochemical Analysis
  • Virus-based gene therapy research
  • Flood Risk Assessment and Management

China Earthquake Administration
2022-2024

National Earthquake Response Support Service
2013-2019

Jinan University
2016

University of Chinese Academy of Sciences
2012-2013

Institute of Geodesy and Geophysics
2011-2013

Chinese Academy of Sciences
2011-2013

Understanding groundwater storage (GWS) changes is vital to the utilization and control of water resources in Tibetan Plateau. However, well level observations are rare this big area, reliable hydrology models including GWS not available. We use hydro-geodesy quantitate Plateau surroundings from 2003 2009 using a combined analysis satellite gravity altimetry data, as model glacial isostatic adjustment (GIA). Release-5 GRACE data jointly used mascon fitting method estimate terrestrial (TWS)...

10.1016/j.epsl.2016.06.002 article EN cc-by-nc-nd Earth and Planetary Science Letters 2016-06-16

The Tibetan Plateau (TP) has the largest number of high-altitude glaciers on Earth. As a source major rivers in Asia, this region provides fresh water to more than one billion people. Any terrestrial storage (TWS) changes there have societal effects large parts continent. Due recent acceleration global warming, part environment TP become drastically unbalanced, with an increased risk disasters. We quantified secular and monthly glacier-mass-balance TWS basins from April 2002 December 2021...

10.3390/rs15143505 article EN cc-by Remote Sensing 2023-07-12

As global warming continues, the monitoring of changes in terrestrial water storage becomes increasingly important since it plays a critical role understanding change and resource management. In North America as elsewhere world, resources strongly impact agriculture animal husbandry. From combination Gravity Recovery Climate Experiment (GRACE) gravity Global Positioning System (GPS) data, is recently found that from August, 2002 to March, 2011 recovered after extreme Canadian Prairies...

10.1016/j.geog.2015.07.002 article EN cc-by-nc-nd Geodesy and Geodynamics 2015-07-01

Time series of the Gravity Recovery and Climate Experiment (GRACE) satellite mission have been successfully used to reveal changes in terrestrial water storage (TWS) many parts world. This has hindered interior Tibetan Plateau since derived TWS there are very sensitive selections different available GRACE solutions, filters remove north-south-oriented (N-S) stripe features observations. resulted controversial distributions previous studies. In this paper, we produce aggregated hydrology...

10.3390/rs14030544 article EN cc-by Remote Sensing 2022-01-24

The aim of this paper is to model and remove the contribution glacial isostatic adjustment (GIA) from observed crustal velocities sea-level rates in East Asia, so that signal other geological processes such as tectonic uplift or global change can be better revealed. State-of-the-art GIA models include 3D variations mantle viscosity lithospheric thickness are employed study. Uncertainties response estimated different ice history background models. It demonstrated uncertainties Asia generally...

10.5047/eps.2011.05.002 article EN cc-by Earth Planets and Space 2011-08-01

We have developed a new glacial isostatic adjustment (GIA) model, RF3L20(β=0. 4) +ICE-4G, which is well constrained by geodetic measurements, relative sea levels and shear-wave seismic tomographic data. Based on this model we will show how GIA affects the secular rate of change gravity level in East Asia. An advantage that viscosities mantle are allowed to vary both radial lateral directions. The laterally homogeneous reference given RF3 (modified from Peltier' s VM2). Lateral viscosity...

10.3969/j.issn.0001-5733.2010.11.007 article EN Chinese Journal of Geophysics 2010-01-01

The Gravity Recovery and Climate Experiment (GRACE) satellite mission measures the combined gravity signal of several overlapping processes. A common approach to separate hydrological in previous ice-covered regions is apply numerical models simulate glacial isostatic adjustment (GIA) signals related vanished ice load then remove them from observed GRACE data. However, results this method are strongly affected by uncertainties viscosity GIA. To avoid this, Wang et al. (Nat Geosci 6(1):38–42,...

10.1186/s40623-018-0804-x article EN cc-by Earth Planets and Space 2018-03-12

The crustal structure under the Tibetan Plateau is quite different from that given by commonly used Preliminary Reference Earth Model (PREM, Dziewonski and Anderson 1981). We investigate effects of such differences on inversion results water trend rates in area using simulated GRACE (Gravity Recovery Climate Experiment) GPS data. When data for inversion, are negligible, confirming validity PREM current even follow-on However, when data, very prominent suggesting an model with a realistic...

10.3319/tao.2012.09.21.01 article EN Terrestrial Atmospheric and Oceanic Sciences 2013-08-01

The crustal structure under the Tibetan Plateau is quite different from that given by commonly used Preliminary Reference Earth Model (PREM, Dziewonski and Anderson 1981).We investigate effects of such differences on inversion results water trend rates in area using simulated GRACE (Gravity Recovery Climate Experiment) GPS data.When data for inversion, are negligible, confirming validity PREM current even follow-on data.However, when data, very prominent suggesting an model with a realistic...

10.3319/tao.2012.09.21.01(tibxs) article EN cc-by Terrestrial Atmospheric and Oceanic Sciences 2013-01-01

We use the average crustal structure of CRUST1.0 model for Tibetan Plateau to establish a realistic earth termed as TC1P, and data from Global Land Data Assimilation System (GLDAS) hydrology Gravity Recovery Climate Experiment (GRACE) data, generate signals assumed in this study. Modeling surface radial displacements gravity variation is performed using both TC1P global Preliminary Reference Earth Model (PREM). Furthermore, inversions based on simulated Positioning (GPS) GRACE are PREM....

10.1016/j.geog.2015.05.002 article EN cc-by-nc-nd Geodesy and Geodynamics 2015-05-01

Land surface water is a key part in the global ecosystem balance and hydrological cycle. Remote sensing has become an effective tool for its spatio-temporal monitoring. However, remote results exemplified so-called indices are subject to several limitations. This paper proposes new index called Sentinel Multi-Band Water Index (SMBWI) extract bodies complex environments from Sentinel-2 satellite imagery. Individual tests explore effectiveness of SMBWI eliminating interference various special...

10.3390/rs16152749 article EN cc-by Remote Sensing 2024-07-27

PDF HTML阅读 XML下载 导出引用 引用提醒 大鲵细胞与大鲵虹彩病毒的微载体规模化培养工艺及优化 DOI: 作者: 作者单位: 1. 华中农业大学水产学院 水生动物医学系, 湖北 武汉 430070;2. 中国水产科学研究院 长江水产研究所, 430223 作者简介: 贾路路(1991-),女,硕士,从事水产动物医学研究.E-mail:1525825924@qq.com 通讯作者: 中图分类号: S941 基金项目: 公益性行业(农业)科研专项(201203086-05). Technologies for large-scale cultivation of giant salamander cells and iridovirus by the Cytodex 3 microcarrier Author: Affiliation: Department Aquatic Animal Medicine, College Fisheries, Huazhong Agricultural University, Wuhan 430070, China;2. Yangtze...

10.3724/sp.j.1118.2018.17058 article EN Journal of Fishery Sciences of China 2018-01-01
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