<?xml version="1.0" encoding="UTF-8" ?>
<VOEvent role="prediction"
	ivorn="ivo://sot.lmsal.com/VOEvent#2007-09-05T19:31:00Z"
	version="1.11"
	xmlns="http://www.ivoa.net/xml/VOEvent/v1.11"
	xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance"
	xmlns:lmsal="http://sot.lmsal.com/lmsal"
	xmlns:crd="urn:nvo-coords"
	xsi:schemaLocation="http://www.ivoa.net/xml/VOEvent/VOEvent-v1.1.xsd">


	<Who>
		<!-- Data pertaining to curation: observer, telescope, instrument, planner, tohbans, ... -->
		<Date>2007-09-05T12:03:40.000Z</Date>    <!-- Time VOEvent was generated. -->
		<PublisherID>http://sot.lmsal.com</PublisherID>

		<Contact>
			<Name>Ted Tarbell</Name>
			<Institution>LMSAL</Institution>
			<Communication>
				<Uri>http://lmsal.com</Uri>
				<AddressLine>3251 Hanover Rd, O/ADBS, B/252, Palo Alto, CA, 94304</AddressLine>
				<Telephone>+1-650-424-2400</Telephone>
				<Email>tarbell@lmsal.com</Email>
			</Communication>		</Contact>

		<lmsal:Telescope>Hinode</lmsal:Telescope>
		<lmsal:Instrument>SOT</lmsal:Instrument>
		<lmsal:Tohbans>Arikawa</lmsal:Tohbans>
		<lmsal:ChiefPlanner>Sakao</lmsal:ChiefPlanner>
		<lmsal:ChiefObserver>Ichimoto</lmsal:ChiefObserver>
	</Who>


	<What>
		<!-- Data pertaining to what was observed, measured, ...   Some of these tags might move into Who section. -->
		<lmsal:obsId></lmsal:obsId>
		<lmsal:OBS_NUM>2</lmsal:OBS_NUM>
		<lmsal:JOP_ID>2</lmsal:JOP_ID>
		<lmsal:JOP></lmsal:JOP>
		<lmsal:JOIN_SB>null</lmsal:JOIN_SB>    <!-- S=SOT, X=XRT, E=EIS, SX=SOT+XRT, EX=EIS+XRT -->
		<lmsal:OBSTITLE>Polar Region Observation</lmsal:OBSTITLE>
		<lmsal:SCI_OBJ>PCH</lmsal:SCI_OBJ>     <!--  Scientific objectives -->
		<lmsal:SCI_OBS>PCH</lmsal:SCI_OBS>     <!-- Objects being observed -->
		<lmsal:NOAA_NUM>NONE</lmsal:NOAA_NUM>
		<lmsal:TARGET>North pole</lmsal:TARGET>
		<lmsal:slotNumber>11</lmsal:slotNumber>
	</What>


	<WhereWhen>
		<!-- Space and Time Coordinates. -->
		<ObservatoryLocation ID="Hinode" />

		<ObservationLocation>
			<lmsal:xCen>0</lmsal:xCen>		<!-- xcen and ycen from FITS -->
			<lmsal:yCen>915</lmsal:yCen>
			<lmsal:xFov>0</lmsal:xFov>
			<lmsal:yFov>0</lmsal:yFov>
			<crd:AstroCoords coord_system_id="UTC-HGS-TOPO">
				<crd:Time>
					<crd:TimeInterval>2007-09-05T19:31:00.000Z 2007-09-06T00:05:30.000Z</crd:TimeInterval>
				</crd:Time>
				<crd:Position3D>0 915</crd:Position3D>
			</crd:AstroCoords>
		</ObservationLocation>

		<Group name="saaIntervals">
			<Param name="saaInterval" value="2007-09-05T19:47:30Z 2007-09-05T20:10:30Z" />
			<Param name="saaInterval" value="2007-09-05T21:25:00Z 2007-09-05T21:48:00Z" />
			<Param name="saaInterval" value="2007-09-05T23:02:30Z 2007-09-05T23:23:30Z" />
		</Group>
	</WhereWhen>


	<Why>
		<!-- Why was observation performed.  Initial scientific assessment, hypothesized mechanisms, classifications, ... -->
		<Concept>
			<lmsal:Goal>Polar Region Observation Campaign</lmsal:Goal>
			<lmsal:Purpose>Na IVDG G-band Ca 1kx2k 2x2</lmsal:Purpose>
		</Concept>

		<Description>
			Daily Note and User Entry:  XRT calibrations: 1) G-band exposures at the 5 pointing positions (10min each, 4 pointings near 4 extreme positions and disk center) to characterize the position of contaminants. 2) Dither-pattern pointings (3 points at the disk center, about 21min) to characterize the X-ray flat-field.  SOT: HOP 25  andnbsp; andnbsp; andnbsp; 07:00UT - 11:30UT@(0,0)  andnbsp; andnbsp; andnbsp; 11:30UT - 15:00UT@(-495,0)   andnbsp; andnbsp; andnbsp; 15:00UT - 18:00UT@(-315,0) andnbsp;  andnbsp; andnbsp; andnbsp; 07:00UT - 12:30UT@(-800, 0)  andnbsp; andnbsp; HOP 02 North pole (6 hours); Request to SOT:  G-band and Ca-H at high cadence full resolution with vector magnetograms.  ??????4.8 x 4 seconds integration time needed in SP to increase the SNR a factor of 2 on the limb Time evolution of granular structures are ~ 1 min. 80""x120"" maps will take 4 hours in total 5 positions (North, South, East, West, disc center) with no active regions. West limb have been only once observed and East limb never !!! At least high resolution G-band maps (1x1) to identify magnetic features.; Scientific Objectives:  ??????Objective: To characterize the temperature, dynamics and statistical distribution of polar coronal jets recently observed by XRT.  Scientific Justification: Recent observations of the north polar coronal hole have shown highly dynamic and frequent (numerous per hour) x-ray jets. This apparently originate from small ephemeral regions within and near the coronal hole boundary. These jets may be the final phase of reconnection; produced when a bi-pole emerges into a predominately open flux region. The previous observations of XRT, taken on 23 November 2006, capture some 44 of these events in a roughly 6 hour period. Estimates of the mass-loading into the IMF based upon a density assumption of 10^9 and volume put the mass flux at just under an order of magnitude of the fast solar wind. These two realizations, the so-called 'Shibata-type' reconnection events and the contribution of mass to the solar wind, are sufficient justification for this observation request.  ??????Motivation: ???ENorth and south limb HINODE/SP data have shown a conspicuous presence of small magnetic fields structures that has not been detected up to now.???EThere is a strong interest in determining the magnetic structure and origin of these magnetic features, besides their relationship among the four cardinal points. ???EDisk center SP data have also shown a opulence of small scale flux tube concentrations with may be connected to north and south poles magnetic activity.; Other Instruments:  UVCS: spectral line intensities for doppler dimming and velocity measurements???@with a slit position orthogonal to solar north CDS: Observations with the 2"" slit using the line list in JOP 146. It would be useful to use the same ;slit positions as EIS. TRACE: 1711 1024 x 1024, Q4 @ 30s cadence with 1600 or 1550 and; WL in context. LASCO: TBD  ??????inner Hinode
		</Description>
	</Why>

</VOEvent>
