<html xmlns:v="urn:schemas-microsoft-com:vml" xmlns:o="urn:schemas-microsoft-com:office:office" xmlns:w="urn:schemas-microsoft-com:office:word" xmlns:m="http://schemas.microsoft.com/office/2004/12/omml" xmlns="http://www.w3.org/TR/REC-html40"><head><meta http-equiv=Content-Type content="text/html; charset=utf-8"><meta name=Generator content="Microsoft Word 15 (filtered medium)"><style><!--
/* Font Definitions */
@font-face
{font-family:Helvetica;
panose-1:2 11 6 4 2 2 2 2 2 4;}
@font-face
{font-family:"Cambria Math";
panose-1:2 4 5 3 5 4 6 3 2 4;}
@font-face
{font-family:DengXian;
panose-1:2 1 6 0 3 1 1 1 1 1;}
@font-face
{font-family:Calibri;
panose-1:2 15 5 2 2 2 4 3 2 4;}
@font-face
{font-family:"\@DengXian";
panose-1:2 1 6 0 3 1 1 1 1 1;}
/* Style Definitions */
p.MsoNormal, li.MsoNormal, div.MsoNormal
{margin:0in;
margin-bottom:.0001pt;
font-size:12.0pt;
font-family:"Times New Roman",serif;}
a:link, span.MsoHyperlink
{mso-style-priority:99;
color:#0563C1;
text-decoration:underline;}
a:visited, span.MsoHyperlinkFollowed
{mso-style-priority:99;
color:#954F72;
text-decoration:underline;}
p.MsoPlainText, li.MsoPlainText, div.MsoPlainText
{mso-style-priority:99;
mso-style-link:"Plain Text Char";
margin:0in;
margin-bottom:.0001pt;
font-size:11.0pt;
font-family:"Calibri",sans-serif;}
p.msonormal0, li.msonormal0, div.msonormal0
{mso-style-name:msonormal;
mso-margin-top-alt:auto;
margin-right:0in;
mso-margin-bottom-alt:auto;
margin-left:0in;
font-size:12.0pt;
font-family:"Times New Roman",serif;}
span.EmailStyle18
{mso-style-type:personal;
font-family:"Calibri",sans-serif;
color:windowtext;}
span.d-none
{mso-style-name:d-none;}
span.comtosotagging
{mso-style-name:co_mto_sotagging;}
span.EmailStyle21
{mso-style-type:personal;
font-family:"Calibri",sans-serif;
color:#1F497D;}
span.EmailStyle22
{mso-style-type:personal-reply;
font-family:"Calibri",sans-serif;
color:#1F497D;}
span.PlainTextChar
{mso-style-name:"Plain Text Char";
mso-style-priority:99;
mso-style-link:"Plain Text";
font-family:"Calibri",sans-serif;}
.MsoChpDefault
{mso-style-type:export-only;
font-size:10.0pt;}
@page WordSection1
{size:8.5in 11.0in;
margin:70.85pt 70.85pt 56.7pt 70.85pt;}
div.WordSection1
{page:WordSection1;}
--></style><!--[if gte mso 9]><xml>
<o:shapedefaults v:ext="edit" spidmax="1026" />
</xml><![endif]--><!--[if gte mso 9]><xml>
<o:shapelayout v:ext="edit">
<o:idmap v:ext="edit" data="1" />
</o:shapelayout></xml><![endif]--></head><body lang=EN-US link="#0563C1" vlink="#954F72"><div class=WordSection1><p class=MsoPlainText>Dear Sir or Madam, <o:p></o:p></p><p class=MsoPlainText><o:p> </o:p></p><p class=MsoPlainText>Could you please advertise a call for abstracts through CEDAR email?<o:p></o:p></p><p class=MsoPlainText>Thank you in advance.<o:p></o:p></p><p class=MsoPlainText><o:p> </o:p></p><p class=MsoPlainText>Regards,<o:p></o:p></p><p class=MsoPlainText>Maosheng<o:p></o:p></p><p class=MsoPlainText>on the behavior of the session conveners (Huixin Liu, Yosuke Yamazaki, Chao Xiong, Jorge Luis Chau)<o:p></o:p></p><p class=MsoPlainText> <o:p></o:p></p><p class=MsoPlainText>###<o:p></o:p></p><p class=MsoPlainText><u>Call for abstracts EGU2020<o:p></o:p></u></p><p class=MsoPlainText>###<o:p></o:p></p><p class=MsoPlainText><o:p> </o:p></p><p class=MsoPlainText>Dear colleagues, dear CEDAR Community,<o:p></o:p></p><p class=MsoPlainText><o:p> </o:p></p><p class=MsoPlainText>We would like to draw your attention to a session on atmosphere-ionosphere coupling at the upcoming EGU General Assembly, in Vienna, Austria, 3-8 May 2020. The details are attached below.<o:p></o:p></p><p class=MsoPlainText>We invite researchers and students to submit your abstracts at <a href="https://meetingorganizer.copernicus.org/EGU2020/abstractsubmission/36063">https://meetingorganizer.copernicus.org/EGU2020/abstractsubmission/36063</a>. The deadline is <b>15 January 2020, 13:00 CET</b>. <o:p></o:p></p><p class=MsoPlainText>We are looking forward to receiving your contributions, and thank you very much for your attention.<o:p></o:p></p><p class=MsoPlainText><o:p> </o:p></p><p class=MsoPlainText>Kind regards,<o:p></o:p></p><p class=MsoPlainText>Maosheng He (Leibniz-IAP)<o:p></o:p></p><p class=MsoPlainText>Huixin Liu(Kyushu University)<o:p></o:p></p><p class=MsoPlainText>Yosuke Yamazaki (GFZ)<o:p></o:p></p><p class=MsoPlainText>Chao Xiong (GFZ)<o:p></o:p></p><p class=MsoPlainText>Jorge Luis Chau(Leibniz-IAP)<o:p></o:p></p><p class=MsoPlainText><o:p> </o:p></p><p class=MsoPlainText><o:p> </o:p></p><p class=MsoPlainText> <o:p></o:p></p><p class=MsoPlainText>###<span style='color:#1F497D'><o:p></o:p></span></p><p class=MsoNormal style='background:white'><span style='font-size:11.5pt;font-family:"Helvetica",sans-serif'>ST3.2<o:p></o:p></span></p><p class=MsoNormal style='background:white'><b><span style='font-size:11.5pt;font-family:"Helvetica",sans-serif;color:#0072BC'>Wave couplings in the atmosphere-ionosphere system<o:p></o:p></span></b></p><p class=MsoNormal style='background:white'><span style='font-size:11.5pt;font-family:"Helvetica",sans-serif'>Convener: Maosheng He <span class=d-none>| </span>Co-conveners: Huixin Liu, Yosuke Yamazaki, Chao Xiong<span class=comtosotagging><b><sup><span style='color:green'>ECS</span></sup></b></span>, Jorge Luis Chau<o:p></o:p></span></p><p class=MsoNormal style='background:white'><span style='font-size:11.5pt;font-family:"Helvetica",sans-serif'><a href="https://meetingorganizer.copernicus.org/EGU2020/abstractsubmission/36063"><span style='color:#0072BC'>Abstract submission</span></a><o:p></o:p></span></p><p class=MsoNormal><span style='font-size:11.5pt;font-family:"Helvetica",sans-serif;background:white'>The atmosphere interacts tightly with its ionized portion, the ionosphere, through a variety of mechanisms, including thermal, fluid dynamical, radiative, electrodynamical, photochemical, and chemical processes. Different combinations of processes dominate different altitude ranges, shaping different atmospheric and ionospheric layers. Atmospheric waves, e.g., gravity waves, tides, and planetary waves, play key roles in the coupling between layers. These waves propagate typically from the lower atmosphere, which are composed of a broad spectrum, spatially ranging from few tens to thousands of kilometers and temporally ranging from few tens of minutes to days. This session invites papers that are related to these waves and their effects on the ionosphere, including modeling as well as observational and theoretical studies.<o:p></o:p></span></p><p class=MsoNormal><span style='font-size:11.0pt;font-family:"Calibri",sans-serif;color:#1F497D'><a href="https://meetingorganizer.copernicus.org/EGU2020/session/36063">https://meetingorganizer.copernicus.org/EGU2020/session/36063</a><o:p></o:p></span></p><p class=MsoNormal><span style='font-size:11.0pt;font-family:"Calibri",sans-serif;color:#1F497D'><o:p> </o:p></span></p></div></body></html>