The D- and E- Regions

The chemistry of the E-region is fairly well understood and even many of the dynamical complications of this region have been successfully modeled on individual bases. Some of the major remaining problems of this region are discussed, in particular the nitric oxide concentration, a gas affecting the...

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1. Verfasser:	Swider, William
Format:	Report
Sprache:	eng
Schlagworte:	Atmospheric Physics D REGION E REGION ION DENSITY ION EXCHANGE IONOSPHERE NITROGEN OXIDES RECOMBINATION REACTIONS SPORADIC E LAYER
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creator	Swider, William
description	The chemistry of the E-region is fairly well understood and even many of the dynamical complications of this region have been successfully modeled on individual bases. Some of the major remaining problems of this region are discussed, in particular the nitric oxide concentration, a gas affecting the ratio of the two major E-region ions, O2(+) and NO(+). The D-region is much simpler than the E-region from a dynamical point of view but extremely much more complex from a chemical standpoint. Recent results from a study of the D-region under bombardment by solar protons is emphasized.
format	Report
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Some of the major remaining problems of this region are discussed, in particular the nitric oxide concentration, a gas affecting the ratio of the two major E-region ions, O2(+) and NO(+). The D-region is much simpler than the E-region from a dynamical point of view but extremely much more complex from a chemical standpoint. Recent results from a study of the D-region under bombardment by solar protons is emphasized.</description><language>eng</language><subject>Atmospheric Physics ; D REGION ; E REGION ; ION DENSITY ; ION EXCHANGE ; IONOSPHERE ; NITROGEN OXIDES ; RECOMBINATION REACTIONS ; SPORADIC E LAYER</subject><creationdate>1974</creationdate><rights>Approved for public release; distribution is unlimited.</rights><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><link.rule.ids>230,776,881,27544,27545</link.rule.ids><linktorsrc>$$Uhttps://apps.dtic.mil/sti/citations/ADA003386$$EView_record_in_DTIC$$FView_record_in_$$GDTIC$$Hfree_for_read</linktorsrc></links><search><creatorcontrib>Swider, William</creatorcontrib><creatorcontrib>AIR FORCE CAMBRIDGE RESEARCH LABS HANSCOM AFB MA</creatorcontrib><title>The D- and E- Regions</title><description>The chemistry of the E-region is fairly well understood and even many of the dynamical complications of this region have been successfully modeled on individual bases. Some of the major remaining problems of this region are discussed, in particular the nitric oxide concentration, a gas affecting the ratio of the two major E-region ions, O2(+) and NO(+). The D-region is much simpler than the E-region from a dynamical point of view but extremely much more complex from a chemical standpoint. Recent results from a study of the D-region under bombardment by solar protons is emphasized.</description><subject>Atmospheric Physics</subject><subject>D REGION</subject><subject>E REGION</subject><subject>ION DENSITY</subject><subject>ION EXCHANGE</subject><subject>IONOSPHERE</subject><subject>NITROGEN OXIDES</subject><subject>RECOMBINATION REACTIONS</subject><subject>SPORADIC E LAYER</subject><fulltext>true</fulltext><rsrctype>report</rsrctype><creationdate>1974</creationdate><recordtype>report</recordtype><sourceid>1RU</sourceid><recordid>eNrjZBANyUhVcNFVSMxLUXDVVQhKTc_MzyvmYWBNS8wpTuWF0twMMm6uIc4euiklmcnxxSWZeakl8Y4ujgYGxsYWZsYEpAGd4hyu</recordid><startdate>19740912</startdate><enddate>19740912</enddate><creator>Swider, William</creator><scope>1RU</scope><scope>BHM</scope></search><sort><creationdate>19740912</creationdate><title>The D- and E- Regions</title><author>Swider, William</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-dtic_stinet_ADA0033863</frbrgroupid><rsrctype>reports</rsrctype><prefilter>reports</prefilter><language>eng</language><creationdate>1974</creationdate><topic>Atmospheric Physics</topic><topic>D REGION</topic><topic>E REGION</topic><topic>ION DENSITY</topic><topic>ION EXCHANGE</topic><topic>IONOSPHERE</topic><topic>NITROGEN OXIDES</topic><topic>RECOMBINATION REACTIONS</topic><topic>SPORADIC E LAYER</topic><toplevel>online_resources</toplevel><creatorcontrib>Swider, William</creatorcontrib><creatorcontrib>AIR FORCE CAMBRIDGE RESEARCH LABS HANSCOM AFB MA</creatorcontrib><collection>DTIC Technical Reports</collection><collection>DTIC STINET</collection></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Swider, William</au><aucorp>AIR FORCE CAMBRIDGE RESEARCH LABS HANSCOM AFB MA</aucorp><format>book</format><genre>unknown</genre><ristype>RPRT</ristype><btitle>The D- and E- Regions</btitle><date>1974-09-12</date><risdate>1974</risdate><abstract>The chemistry of the E-region is fairly well understood and even many of the dynamical complications of this region have been successfully modeled on individual bases. Some of the major remaining problems of this region are discussed, in particular the nitric oxide concentration, a gas affecting the ratio of the two major E-region ions, O2(+) and NO(+). The D-region is much simpler than the E-region from a dynamical point of view but extremely much more complex from a chemical standpoint. Recent results from a study of the D-region under bombardment by solar protons is emphasized.</abstract><oa>free_for_read</oa></addata></record>
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subjects	Atmospheric Physics D REGION E REGION ION DENSITY ION EXCHANGE IONOSPHERE NITROGEN OXIDES RECOMBINATION REACTIONS SPORADIC E LAYER
title	The D- and E- Regions
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