Platforms: Cryosat-2 - Revision history

Roman at 12:05, 3 December 2012

Roman — Mon, 03 Dec 2012 12:05:30 GMT

← Older revision		Revision as of 12:05, 3 December 2012
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	{\|		{\|
	\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]		\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]
-	\| CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.\|	+	\| CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.
	\|}		\|}

Roman — Mon, 03 Dec 2012 12:05:21 GMT

← Older revision		Revision as of 12:05, 3 December 2012
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	{\|		{\|
	\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]		\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]
-	\|~~{{al=c}}~~ CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.\|	+	\| CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.\|
	\|}		\|}

Roman — Mon, 03 Dec 2012 12:04:45 GMT

← Older revision		Revision as of 12:04, 3 December 2012
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	{\|		{\|
	\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]		\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]
-	\|{{va=~~top~~}} CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.\|	+	\|{{al=c}} CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.\|
	\|}		\|}

Roman — Mon, 03 Dec 2012 12:04:33 GMT

← Older revision		Revision as of 12:04, 3 December 2012
Line 7:		Line 7:
	{\|		{\|
	\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]		\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]
-	\|{{va=t}} CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.\|	+	\|{{va=top}} CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.\|
	\|}		\|}

Roman — Mon, 03 Dec 2012 12:03:26 GMT

← Older revision		Revision as of 12:03, 3 December 2012
Line 7:		Line 7:
	{\|		{\|
	\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]		\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]
-	\|{{va=t}} CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.	+	\|{{va=t}} CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.\|
	\|}		\|}

Roman — Mon, 03 Dec 2012 12:02:16 GMT

← Older revision		Revision as of 12:02, 3 December 2012
Line 7:		Line 7:
	{\|		{\|
	\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]		\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]
-	\| CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.	+	\|{{va=t}} CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.
	\|}		\|}

Roman — Mon, 03 Dec 2012 12:00:08 GMT

← Older revision		Revision as of 12:00, 3 December 2012
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	{\|		{\|
	\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]		\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]
-	\|~~{{^}}~~ CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.	+	\| CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.
	\|}		\|}

Roman — Mon, 03 Dec 2012 11:59:53 GMT

← Older revision		Revision as of 11:59, 3 December 2012
Line 7:		Line 7:
	{\|		{\|
	\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]		\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]
-	\|\|^ CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.	+	\|{{^}} CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.
	\|}		\|}

Roman — Mon, 03 Dec 2012 11:59:33 GMT

← Older revision		Revision as of 11:59, 3 December 2012
Line 7:		Line 7:
	{\|		{\|
	\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]		\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]
-	\|^ CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.	+	\|\|^ CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.
	\|}		\|}

Roman — Mon, 03 Dec 2012 11:59:28 GMT

← Older revision		Revision as of 11:59, 3 December 2012
Line 7:		Line 7:
	{\|		{\|
	\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]		\|[[File:Cryosat2.jpg\|thumb\|left\|200px]]
-	\|{^}CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.	+	\|^ CryoSat’s radar altimeter can sense the gravity field at the ocean surface,<br>so that seafloor characteristics at scales of 5–10 km are revealed.
	\|}		\|}