• 文献检索
  • 文档翻译
  • 深度研究
  • 学术资讯
  • Suppr Zotero 插件Zotero 插件
  • 邀请有礼
  • 套餐&价格
  • 历史记录
应用&插件
Suppr Zotero 插件Zotero 插件浏览器插件Mac 客户端Windows 客户端微信小程序
定价
高级版会员购买积分包购买API积分包
服务
文献检索文档翻译深度研究API 文档MCP 服务
关于我们
关于 Suppr公司介绍联系我们用户协议隐私条款
关注我们

Suppr 超能文献

核心技术专利:CN118964589B侵权必究
粤ICP备2023148730 号-1Suppr @ 2026

文献检索

告别复杂PubMed语法,用中文像聊天一样搜索,搜遍4000万医学文献。AI智能推荐,让科研检索更轻松。

立即免费搜索

文件翻译

保留排版,准确专业,支持PDF/Word/PPT等文件格式,支持 12+语言互译。

免费翻译文档

深度研究

AI帮你快速写综述,25分钟生成高质量综述,智能提取关键信息,辅助科研写作。

立即免费体验

使用可变随机游走过程噪声改进全球定位系统对流层路径延迟估计

Improved GPS tropospheric path delay estimation using variable random walk process noise.

作者信息

Young Zachary M, Blewitt Geoffrey, Kreemer Corné

机构信息

Nevada Bureau of Mines and Geology, University of Nevada, 1664 N Virginia St. MS 178, Reno, NV 89557 USA.

Department of Geosciences, University of Montana, 32 Campus Dr., Missoula, MT 59812 USA.

出版信息

J Geod. 2024;98(10):89. doi: 10.1007/s00190-024-01898-3. Epub 2024 Oct 7.

DOI:10.1007/s00190-024-01898-3
PMID:39386935
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11458690/
Abstract

UNLABELLED

Accurate positioning using the Global Positioning System relies on accurate modeling of tropospheric delay. Estimated tropospheric delay must vary sufficiently to capture true variations; otherwise, systematic errors propagate into estimated positions, particularly the vertical. However, if the allowed delay variation is too large, the propagation of data noise into all parameters is amplified, reducing precision. Here we investigate the optimal choice of tropospheric constraints applied in the GipsyX software, which are specified by values of random walk process noise. We use the variability of 5-min estimated positions as a proxy for tropospheric error. Given that weighted mean 5-min positions closely replicate 24-h solutions, our ultimate goal is to improve 24-h positions and other daily products, such as precise orbit parameters. The commonly adopted default constraint for the zenith wet delay (ZWD) is 3 mm/√(hr) for 5-min data intervals. Using this constraint, we observe spurious wave-like patterns of 5-min vertical displacement estimates with amplitudes ~ 100 mm coincident with Winter Storm Ezekiel of November 27, 2019, across the central/eastern USA. Loosening the constraint suppresses the spurious waves and reduces 5-min vertical displacement variability while improving water vapor estimates. Further improvement can be achieved when optimizing constraints regionally, or for each station. Globally, results are typically optimized in the range of 6-12 mm/√(hr). Generally, we at least recommend loosening the constraint from the current default of 3 mm/√(hr) to 6 mm/√(hr) for ZWD every 300 s. Constraint values must be scaled by √(/300) for alternative data intervals of seconds.

SUPPLEMENTARY INFORMATION

The online version contains supplementary material available at 10.1007/s00190-024-01898-3.

摘要

未标注

使用全球定位系统进行精确定位依赖于对流层延迟的精确建模。估计的对流层延迟必须有足够的变化以捕捉真实变化;否则,系统误差会传播到估计位置,尤其是垂直方向。然而,如果允许的延迟变化太大,数据噪声向所有参数的传播会被放大,从而降低精度。在这里,我们研究了在GipsyX软件中应用的对流层约束的最佳选择,这些约束由随机游走过程噪声值指定。我们使用5分钟估计位置的变异性作为对流层误差的代理。鉴于加权平均5分钟位置能紧密复制24小时解,我们的最终目标是改善24小时位置和其他每日产品,如精确轨道参数。对于天顶湿延迟(ZWD),常用的默认约束是在5分钟数据间隔内为3毫米/√(小时)。使用这个约束,我们观察到2019年11月27日冬季风暴以西结期间,美国中部/东部5分钟垂直位移估计出现了虚假的波状模式,振幅约为100毫米。放宽约束可抑制虚假波,并减少5分钟垂直位移变异性,同时改善水汽估计。在区域或每个站点优化约束时可进一步改善。在全球范围内,结果通常在6 - 12毫米/√(小时)范围内得到优化。一般来说,我们至少建议将ZWD每300秒的约束从当前默认的3毫米/√(小时)放宽到6毫米/√(小时)。对于秒的替代数据间隔,约束值必须乘以√(/300)进行缩放。

补充信息

在线版本包含可在10.1007/s00190-024-01898-3获取的补充材料。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/3a08134e669c/190_2024_1898_Fig17_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/f4511763b701/190_2024_1898_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/662373b18922/190_2024_1898_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/a4c4fb2c5f2f/190_2024_1898_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/1fc5b3c3257e/190_2024_1898_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/6e0575e8169a/190_2024_1898_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/855f611c7fc9/190_2024_1898_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/583f32e8c876/190_2024_1898_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/569f6ccbc867/190_2024_1898_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/54b0682e990f/190_2024_1898_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/e0f202c3ff69/190_2024_1898_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/be96be37cc44/190_2024_1898_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/5b61a491c82e/190_2024_1898_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/544b9967d588/190_2024_1898_Fig13_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/d6ae2af00115/190_2024_1898_Fig14_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/c53522a0b8dd/190_2024_1898_Fig15_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/1258209b5637/190_2024_1898_Fig16_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/3a08134e669c/190_2024_1898_Fig17_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/f4511763b701/190_2024_1898_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/662373b18922/190_2024_1898_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/a4c4fb2c5f2f/190_2024_1898_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/1fc5b3c3257e/190_2024_1898_Fig4_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/6e0575e8169a/190_2024_1898_Fig5_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/855f611c7fc9/190_2024_1898_Fig6_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/583f32e8c876/190_2024_1898_Fig7_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/569f6ccbc867/190_2024_1898_Fig8_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/54b0682e990f/190_2024_1898_Fig9_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/e0f202c3ff69/190_2024_1898_Fig10_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/be96be37cc44/190_2024_1898_Fig11_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/5b61a491c82e/190_2024_1898_Fig12_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/544b9967d588/190_2024_1898_Fig13_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/d6ae2af00115/190_2024_1898_Fig14_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/c53522a0b8dd/190_2024_1898_Fig15_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/1258209b5637/190_2024_1898_Fig16_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/66eb/11458690/3a08134e669c/190_2024_1898_Fig17_HTML.jpg

相似文献

1
Improved GPS tropospheric path delay estimation using variable random walk process noise.使用可变随机游走过程噪声改进全球定位系统对流层路径延迟估计
J Geod. 2024;98(10):89. doi: 10.1007/s00190-024-01898-3. Epub 2024 Oct 7.
2
Evaluation of the ZWD/ZTD Values Derived from MERRA-2 Global Reanalysis Products Using GNSS Observations and Radiosonde Data.利用全球导航卫星系统(GNSS)观测数据和探空仪数据对来自MERRA-2全球再分析产品的天顶湿延迟(ZWD)/天顶总延迟(ZTD)值进行评估
Sensors (Basel). 2020 Nov 11;20(22):6440. doi: 10.3390/s20226440.
3
Kinematic Zenith Tropospheric Delay Estimation with GNSS PPP in Mountainous Areas.山区 GNSS PPP 动态天顶对流层延迟估计。
Sensors (Basel). 2021 Aug 25;21(17):5709. doi: 10.3390/s21175709.
4
Sensitivity of Shipborne GNSS Estimates to Processing Modeling Based on Simulated Dataset.基于模拟数据集的舰载全球导航卫星系统(GNSS)估计对处理建模的敏感性
Sensors (Basel). 2023 Jul 22;23(14):6605. doi: 10.3390/s23146605.
5
Precise Point Positioning on the Reliable Detection of Tropospheric Model Errors.基于对流层模型误差可靠检测的精确点位定位
Sensors (Basel). 2020 Mar 14;20(6):1634. doi: 10.3390/s20061634.
6
A New Zenith Tropospheric Delay Grid Product for Real-Time PPP Applications over China.一种适用于中国实时精密单点定位应用的新型天顶对流层延迟格网产品。
Sensors (Basel). 2017 Dec 27;18(1):65. doi: 10.3390/s18010065.
7
Analysing the Zenith Tropospheric Delay Estimates in On-line Precise Point Positioning (PPP) Services and PPP Software Packages.分析在线精密单点定位(PPP)服务和PPP软件包中的天顶对流层延迟估计值。
Sensors (Basel). 2018 Feb 14;18(2):580. doi: 10.3390/s18020580.
8
Assessment and Validation of Small-Scale Tropospheric Delay Estimations Based on NWP Data.基于数值天气预报(NWP)数据的对流层小尺度延迟估计的评估与验证
Sensors (Basel). 2024 Oct 12;24(20):6579. doi: 10.3390/s24206579.
9
Evaluation of Empirical Tropospheric Models Using Satellite-Tracking Tropospheric Wet Delays with Water Vapor Radiometer at Tongji, China.利用中国同济大学的水汽辐射计通过卫星跟踪对流层湿延迟评估经验对流层模型
Sensors (Basel). 2016 Feb 2;16(2):186. doi: 10.3390/s16020186.
10
Assessment of Three Tropospheric Delay Models (IGGtrop, EGNOS and UNB3m) Based on Precise Point Positioning in the Chinese Region.基于中国区域精密单点定位对三种对流层延迟模型(IGGtrop、EGNOS和UNB3m)的评估
Sensors (Basel). 2016 Jan 20;16(1):122. doi: 10.3390/s16010122.

本文引用的文献

1
Unravelling the contribution of early postseismic deformation using sub-daily GNSS positioning.利用亚日GNSS定位揭示震后早期变形的贡献。
Sci Rep. 2019 Feb 11;9(1):1775. doi: 10.1038/s41598-019-39038-z.
2
Estimating zenith tropospheric delays from BeiDou navigation satellite system observations.利用北斗导航卫星系统观测值估计天顶对流层延迟。
Sensors (Basel). 2013 Apr 3;13(4):4514-26. doi: 10.3390/s130404514.