Lesson 3 of 4 · Haiyang ocean observation
Haiyang: choose the measurement for the ocean question
8 minute lesson · 3 checks along the way
Your goal for this lessonDistinguish ocean color, surface dynamics and the supporting data-quality information.
In this lesson 3 sections · 3 checks
Using archive links & definitions
Follow a linked name to explore its archive card. “Back to your lesson” brings you to the same part of the reading.
Words with a dotted underline open a short definition right here in the lesson.
Read & understand
One family, several observing jobs
Haiyang is China’s ocean-observation satellite family. HY-1 missions emphasize optical observations such as ocean color, while HY-2 uses microwave measurements for ocean dynamics, including surface height and wind. The distinction follows the physical quantity being measured rather than a ranking in which a higher mission number is always better. Different observations can contribute to the same environmental question.
The current National Satellite Ocean Application Service directory identifies HY-3A with the alternate designation HY-1E as an ocean-color mission. Older development descriptions assigned other capabilities to future HY-3 concepts, so a family number alone is not reliable evidence of the flown instrument. Check the specific spacecraft and product. The directory also publishes data-gap notices, reminding users that an available mission name does not guarantee an uninterrupted usable record.
Check 1 of 3
10 pointsUse the reading above. You can try again without losing points.
Read & understand
From radiance or range to an interpreted product
Ocean-color instruments observe light in different wavelength bands. Atmospheric correction and a retrieval method connect those measurements to quantities such as chlorophyll concentration; water color alone is not a direct count of organisms. Microwave instead uses ranging and precise orbital knowledge to estimate surface height. CNES contributes DORIS orbit-determination instruments to selected HY-2 missions, illustrating why a surface measurement also depends on knowing the observing spacecraft’s position.
For an invented altimetry example, let the satellite be 1,000,000 metres above a defined reference surface. A corrected vertical range of 999,998 metres places the observed surface two metres above that reference. If the orbit height is mistakenly raised by one metre while the range stays unchanged, the inferred surface height also rises by one metre. This simplified subtraction excludes the detailed corrections of real altimetry; it shows how orbit error can enter a geophysical result.
Identify the observable before combining products
Original teaching diagram. OPTICAL OBSERVATIONS. Light across wavelength bands. Color-related retrievals. MICROWAVE OBSERVATIONS. Range and radar response. Height or wind retrievals. A simplified height estimate needs both corrected range and precise satellite position.
Open full-size diagram in a new tab: Identify the observable before combining productsOrbView-2 SeaWiFS observation of the Okavango Delta on 28 March 1999. The dark borders are map annotations. This different mission’s processed image illustrates color-observation interpretation; it is not Haiyang data or a surface-height map.
Look closely
Does a dark border in this image show a physical structure measured by the sensor?
See what to notice
No. The boundaries are overlaid cartographic annotations. They help locate the image but must be distinguished from the observed surface and clouds.
Check 2 of 3
10 pointsUse the reading above. You can try again without losing points.
Read & understand
Read the image and its limits
The archive’s OrbView-2 SeaWiFS view of the Okavango Delta is a processed observation from a different mission. Its overlaid borders are map annotations rather than objects seen by the sensor. The scene is useful for examining how a color instrument represents water, land and clouds; it is not a Haiyang observation, an ocean-height map or a direct chlorophyll measurement for every colored pixel.
Suppose a fictional optical product has a cloud-covered area while a microwave product has valid samples nearby. The second can add evidence without filling the first product’s exact missing quantity. Compare dates, units, footprints and quality flags before combining them. Haiyang’s wider value comes from a system of complementary sensors, orbit determination and data services, with the limitations of each product preserved in the explanation.
Check 3 of 3
10 pointsUse the reading above. You can try again without losing points.
Put it together
Your lesson progress
Each check connects to a part of the story. Complete all 3 to earn your 25-point lesson bonus.
Explore further · Optional
Go to the source
Explore the evidence behind this lesson. These optional readings and videos open in a new tab.
- Read: NSOAS: Chinese ocean-satellite data and mission directoryThe current directory distinguishes color, dynamics and surveillance products and labels HY-3A as HY-1E. Data-gap notices are not interpreted as whole-mission failures.
- Read: CNES: Haiyang and French HY-2 contributionsUse instrument and orbit-determination roles. Future HY-2E/F dates on this page remain forecasts.
- Read: CAS: HY-2 ocean-dynamics mission in 2011The article is dated August 2011 despite its later URL path. Its HY-3 forecast is not current mission history.
- Read: SeaWiFS project: Okavango Delta observationA processed OrbView-2/SeaWiFS image of 28 March 1999, with overlaid borders; it is a comparison, not Haiyang data.