How does the aurora heat the upper atmosphere?
极光如何加热高层大气?
基本信息
- 批准号:NE/S015167/1
- 负责人:
- 金额:$ 67.51万
- 依托单位:
- 依托单位国家:英国
- 项目类别:Fellowship
- 财政年份:2019
- 资助国家:英国
- 起止时间:2019 至 无数据
- 项目状态:未结题
- 来源:
- 关键词:
项目摘要
My research will study the aurora, a beautiful display caused by energetic particles from space hitting the Earth's atmosphere at about 40 million mph. The aurora typically deposits 50 GW of power into the atmosphere, comparable to the electricity consumption of the UK. This huge energy source has considerable influence on the temperature and composition of the upper atmosphere, particularly in polar regions. The aurora is therefore one of many ingredients needed for computer simulations of the whole atmosphere, which predict changes to Earth's climate and to concentrations of gases such as ozone.Intense currents flow within and around aurora, heating the atmosphere just as an electric current heats a resistor. This heating has dramatic effects on the upper atmosphere, but several fundamental aspects remain undetermined. Previously it has been very difficult to measure the temperature of the atmosphere at auroral heights; it is too high for weather balloons, but too low for spacecraft. However, I recently made the exciting discovery, through experiment and theory, that the ratio of brightnesses of two specific auroral colours depends on the temperature of the atmosphere; therefore by observing these wavelengths in the aurora we can calculate the temperature. My idea is to use extremely sensitive cameras equipped with colour filters to make maps of atmospheric temperature, just like a thermal imaging camera. These temperature maps can be combined with radar measurements of the upper atmosphere to estimate the electrical conductivity, which is an important property influencing the flow of electric current through near-Earth space and the atmosphere. A computer simulation will help me to understand how different types of aurora are produced, what electric currents they generate, and how the aurora affects the temperature and chemistry of the upper atmosphere.
我的研究将研究极光,这是一种美丽的显示,是由来自太空的高能粒子以每小时4000万英里的速度撞击地球大气层造成的。极光通常会向大气中沉积50吉瓦的电力,相当于英国的电力消耗。这种巨大的能源对高层大气的温度和组成有相当大的影响,特别是在极地地区。因此,极光是计算机模拟整个大气层所需的众多成分之一,这些成分可以预测地球气候和臭氧等气体浓度的变化。极光内部和周围有强烈的电流流动,加热大气层,就像电流加热电阻器一样。这种加热对高层大气产生了巨大的影响,但几个基本方面仍然没有确定。以前,测量极光高度的大气温度非常困难;它对气象气球来说太高,但对航天器来说又太低。然而,我最近通过实验和理论取得了令人兴奋的发现,即两种特定极光颜色的亮度比率取决于大气温度;因此,通过观察极光中的这些波长,我们可以计算温度。我的想法是使用配备彩色滤光片的极敏感相机来绘制大气温度图,就像热成像相机一样。这些温度图可与高层大气的雷达测量相结合,以估计电导率,电导率是影响电流在近地空间和大气中流动的一个重要特性。计算机模拟将帮助我了解不同类型的极光是如何产生的,它们产生什么电流,以及极光如何影响高层大气的温度和化学成分。
项目成果
期刊论文数量(10)
专著数量(0)
科研奖励数量(0)
会议论文数量(0)
专利数量(0)
Multiscale Observation of Two Polar Cap Arcs Occurring on Different Magnetic Field Topologies
- DOI:10.1029/2019ja027611
- 发表时间:2020-08
- 期刊:
- 影响因子:0
- 作者:J. Reidy;J. Reidy;R. Fear;D. Whiter;B. Lanchester;A. Kavanagh;Daniel J. Price;J. Chadney;Yongliang Zhang;L. Paxton
- 通讯作者:J. Reidy;J. Reidy;R. Fear;D. Whiter;B. Lanchester;A. Kavanagh;Daniel J. Price;J. Chadney;Yongliang Zhang;L. Paxton
Diffuse and Pulsating Aurora
- DOI:10.1007/s11214-019-0629-3
- 发表时间:2020-01
- 期刊:
- 影响因子:10.3
- 作者:Y. Nishimura;M. Lessard;Y. Katoh;Y. Miyoshi;E. Grono;N. Partamies;Nithin Sivadas;K. Hosokawa;M. Fukizawa;M. Samara;R. Michell;R. Kataoka;T. Sakanoi;D. Whiter;S. Oyama;Y. Ogawa;S. Kurita
- 通讯作者:Y. Nishimura;M. Lessard;Y. Katoh;Y. Miyoshi;E. Grono;N. Partamies;Nithin Sivadas;K. Hosokawa;M. Fukizawa;M. Samara;R. Michell;R. Kataoka;T. Sakanoi;D. Whiter;S. Oyama;Y. Ogawa;S. Kurita
Fine-Scale Electric Fields and Joule Heating From Observations of the Aurora
极光观测中的精细电场和焦耳热
- DOI:10.1029/2022ja030628
- 发表时间:2023
- 期刊:
- 影响因子:0
- 作者:Krcelic P
- 通讯作者:Krcelic P
Morphological evolution and spatial profile changes of poleward moving auroral forms
- DOI:10.5194/angeo-41-115-2023
- 发表时间:2023-03
- 期刊:
- 影响因子:1.9
- 作者:A. Goertz;N. Partamies;D. Whiter;L. Baddeley
- 通讯作者:A. Goertz;N. Partamies;D. Whiter;L. Baddeley
Characteristics of fragmented aurora-like emissions (FAEs) observed on Svalbard
在斯瓦尔巴群岛观测到的碎片状极光发射(FAE)的特征
- DOI:10.5194/angeo-39-277-2021
- 发表时间:2021
- 期刊:
- 影响因子:1.9
- 作者:Dreyer J
- 通讯作者:Dreyer J
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Daniel Whiter其他文献
3D current system of eastward expanding auroral surges
向东扩展的极光涌流的 3D 电流系统
- DOI:
- 发表时间:
2018 - 期刊:
- 影响因子:0
- 作者:
Yoshimasa Tanaka;Yasunobu Ogawa;Akira Kadokura;Bjorn Gustavsson;Noora Partamies;Kirsti Kauristie;Daniel Whiter;Carl-fredrik Enell;Urban Brandstrom;Tima Sergienko;Alexander Kozlovsky;Heikki Vanhamaki;Akimasa Yoshikawa;Hiroshi Miyaoka - 通讯作者:
Hiroshi Miyaoka
オーロラプロファイルと電子密度プロファイル
极光剖面和电子密度剖面
- DOI:
- 发表时间:
2016 - 期刊:
- 影响因子:0
- 作者:
田中良昌;小川泰信;門倉昭;Bjoumlrn Gustavsson;Kirsti Kauristie;Daniel Whiter;Carl-Fredrik Enell;Urban Braumlndstroumlm;Tima Sergienko;Alexandre Kozlovsky;Noora Partamies;Hiroshi Miyaoka;and Michael Kosch - 通讯作者:
and Michael Kosch
東向き伝搬性オーロラ渦のトモグラフィ解析
向东传播的极光涡旋的层析分析
- DOI:
- 发表时间:
2015 - 期刊:
- 影响因子:0
- 作者:
田中 良昌;小川 泰信;門倉 昭;Bjorn Gustavsson;Noora Partamies;Daniel Whiter;Carl-Fredrik Enell;Urban Braendstroem;宮岡 宏;Alexander Kozlovsky - 通讯作者:
Alexander Kozlovsky
Eastward-expanding auroral surges observed in the post-midnight sector during a multiple-onset substorm
在多次发作的亚暴期间,在午夜后区域观察到向东扩展的极光激增
- DOI:
10.1186/s40623-015-0350-8 - 发表时间:
2015 - 期刊:
- 影响因子:0
- 作者:
Yoshimasa Tanaka;Yasunobu Ogawa;Akira Kadokura;Noora Partamies;Daniel Whiter;Carl-Fredrik Enell;Urban Brändström;Tima Sergienko;Björn Gustavsson;Alexander Kozlovsky;Hiroshi Miyaoka;and Akimasa Yoshikawa - 通讯作者:
and Akimasa Yoshikawa
電離圏電気伝導度を算出するための衝突周波数
用于计算电离层电导率的碰撞频率
- DOI:
- 发表时间:
2019 - 期刊:
- 影响因子:0
- 作者:
Akimasa Ieda;Kirsti Kauristie;Yukitoshi Nishimura;Yukinaga Miyashita;Harald U. Frey ;Liisa Juusola;Daniel Whiter;Masahito Nose;Matthew O. Fillingim;Farideh Honary;Neil C. Rogers ;Yoshizumi Miyoshi;Tsubasa Miura;Takahiro Kawashima and Shinobu ;家田 章正 - 通讯作者:
家田 章正
Daniel Whiter的其他文献
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{{ truncateString('Daniel Whiter', 18)}}的其他基金
EISCAT_3D: Fine-scale structuring, scintillation, and electrodynamics (FINESSE)
EISCAT_3D:精细结构、闪烁和电动力学 (FINESSE)
- 批准号:
NE/W003007/1 - 财政年份:2022
- 资助金额:
$ 67.51万 - 项目类别:
Research Grant
Variability of neutral temperature in the high-latitude upper atmosphere
高纬度高层大气中性温度的变化
- 批准号:
NE/N004051/1 - 财政年份:2016
- 资助金额:
$ 67.51万 - 项目类别:
Research Grant
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