极地研究
極地研究
겁지연구
CHINESE JOURNAL OF POLAR RESEARCH
2014年
3期
316-323
,共8页
徐彤%徐彬%吴健%胡艳莉%许正文
徐彤%徐彬%吳健%鬍豔莉%許正文
서동%서빈%오건%호염리%허정문
电离层加热%抗磁性电流%极低频波%极区电急流
電離層加熱%抗磁性電流%極低頻波%極區電急流
전리층가열%항자성전류%겁저빈파%겁구전급류
ionospheric heating%diamagnetic current%extremely low frequency waves%polar electrojet
“极区电急流天线”辐射依赖于低电离层D/E区背景电急流,而高电离层F区极低频调制加热,可产生抗磁性电流,形成极低频波辐射源。利用电离层F区一维时变加热数值模型,采用全波解算法研究高纬Troms?(69.59°N,19.23°E)地区电离层F区极低频调制加热。模拟结果表明,极区高电离层激发的极低频波与极区低电离层激发的结果不同。加热泵波的有效辐射功率( effective radiated power ,ERP)、调制频率及电离层背景对极低频波强度有着重要影响。
“極區電急流天線”輻射依賴于低電離層D/E區揹景電急流,而高電離層F區極低頻調製加熱,可產生抗磁性電流,形成極低頻波輻射源。利用電離層F區一維時變加熱數值模型,採用全波解算法研究高緯Troms?(69.59°N,19.23°E)地區電離層F區極低頻調製加熱。模擬結果錶明,極區高電離層激髮的極低頻波與極區低電離層激髮的結果不同。加熱泵波的有效輻射功率( effective radiated power ,ERP)、調製頻率及電離層揹景對極低頻波彊度有著重要影響。
“겁구전급류천선”복사의뢰우저전리층D/E구배경전급류,이고전리층F구겁저빈조제가열,가산생항자성전류,형성겁저빈파복사원。이용전리층F구일유시변가열수치모형,채용전파해산법연구고위Troms?(69.59°N,19.23°E)지구전리층F구겁저빈조제가열。모의결과표명,겁구고전리층격발적겁저빈파여겁구저전리층격발적결과불동。가열빙파적유효복사공솔( effective radiated power ,ERP)、조제빈솔급전리층배경대겁저빈파강도유착중요영향。
Polar ionospheric heaters operated by HARRP and EISCAT have generated extremely low frequency waves by modulating the auroral electrojet at D and E region altitudes .However , the auroral electrojet often varies over time and is not always present .Alternatively, modulated F-region HF heating can generate ionospheric diamagnetic cur-rent, and the periodic modulation results in a magnetic moment that radiates extremely low frequency waves .Based on a one-dimensional time physical model of polar ionospheric heating and a full-wave model , we analyzed the fea-tures of extremely low frequency waves over Troms?(69.59°N, 19.23°E).The results showed that extremely low frequency waves on the ground are different from lower ionospheric modulation , i.e., radiation of polar electrojet antenna.Furthermore, effective radiated power (ERP), modulated frequency, and ionospheric background, have significant influence on the generated extremely low frequency wave .