View source for Engineering:Nimbus program

{{Short description|Second-generation U.S. robotic spacecraft}}
{{Infobox spacecraft class
| image =Nimbus rendering.jpg 
| caption =Artist's drawing of the general design of the Nimbus series of satellites. The solar-panel "wings" move throughout the day to track the Sun during the daylight part of the satellite's orbit. The 10-foot-tall satellite has the attitude control system on top, separated from a 5-foot-diameter "sensory ring" (center) with scaffolding. The sensory ring holds the batteries and electronics for each of the sensors that are mounted underneath the ring (bottom). 
| name = Nimbus
| manufacturer = [[Company:General Electric|General Electric]]<br>RCA Astro
| country = {{wipe|United States}}
| bus = 
| applications = [[Engineering:Weather satellite|Weather]]
| orbits = [[Astronomy:Low Earth orbit|Low Earth]]
| operator = [[Organization:NASA|NASA]]
| lifetime = 
| derivedfrom = 
| derivatives = <!--spacecraft classes derived from it (not using it)-->
| Preceded = <!--spacecraft class preceding-->
| Succeeded = <!--spacecraft class succeeding-->

<!--Production-->
| status = Disabled
| built = 8
| orders =
| launched = 
| operational = 
| retired = 
| failed = 1
| lost = 
| first = [[Engineering:Nimbus 1|Nimbus 1]]
| last = [[Engineering:Nimbus 7|Nimbus 7]]
|imsize=|image_caption=Artist's drawing of the general design of the Nimbus series of satellites. The solar-panel "wings" move throughout the day to track the Sun during the daylight part of the satellite's orbit. The 10-foot-tall satellite has the attitude control system on top, separated from a 5-foot-diameter "sensory ring" (center) with scaffolding. The sensory ring holds the batteries and electronics for each of the sensors that are mounted underneath the ring (bottom).}}

The '''Nimbus''' [[Astronomy:Satellite|satellite]]s were second-generation U.S. [[Engineering:Robotic spacecraft|robotic spacecraft]] launched between 1964 and 1978 used for [[Physics:Meteorology|meteorological]] research and development. The spacecraft were designed to serve as stabilized, Earth-oriented platforms for the testing of advanced systems to sense and collect [[Physics:Atmospheric sciences|atmospheric science]] data. Seven Nimbus spacecraft have been launched into near-polar, [[Astronomy:Sun-synchronous orbit|Sun-synchronous orbit]]s beginning with Nimbus 1 on August 28, 1964. On board the Nimbus satellites are various instrumentation for imaging, sounding, and other studies in different spectral regions.  The Nimbus satellites were launched aboard [[Engineering:Thor-Agena|Thor-Agena rockets]] (Nimbus 1–4) and [[Engineering:Delta (rocket family)|Delta rockets]] (Nimbus 5–7).

Over a 20-year period from the launch of the first satellite, the Nimbus series of missions was the United States' primary research and development platform for satellite [[Earth:Remote sensing|remote sensing]] of the Earth. The seven Nimbus satellites, launched over a fourteen-year period, shared their space-based observations of the planet for thirty years. NASA transferred the technology tested and refined by the Nimbus missions to the [[Organization:National Oceanic and Atmospheric Administration|National Oceanic and Atmospheric Administration]] (NOAA) for its operational satellite instruments. The technology and lessons learned from the Nimbus missions are the heritage of most of the Earth-observing satellites NASA and NOAA have launched over the past three decades.<ref>{{cite web | url=http://earthobservatory.nasa.gov/Study/Nimbus/ | title=Nimbus: 40th Anniversary | first=Rebecca | last=Lindsey | date=July 19, 2005 | publisher=[[Astronomy:NASA Earth Observatory|NASA Earth Observatory]] | access-date=2006-05-16}}</ref>

==Contributions==

===Weather forecasting===
{| class="simple" style="width: 35%; margin-left:0.5em; text-align: center" border="1" align="right"
|- bgcolor="#CCF"
!colspan="3"|NASA's Nimbus contractors<ref>[https://archive.org/stream/missilesrockets8196unse#page/n669/mode/2up ''Missiles and Rockets''], March 13, 1961, p. 34.</ref>
|- bgcolor="#EBEBFF"
!Company||System||Amount*
|-
|rowspan="3"|'''[[Company:General Electric|General Electric]]'''||Prime||$2,100,000
|-
|Control & stabilization||1,515,710
|-
|5-watt transmitter||92,652
|-
|rowspan="2"|'''[[Company:RCA|RCA]]'''||Cameras & solar power||302,324
|-
|Vidicon and solar power||{{N/A}}
|-
|'''IT&T Labs'''||High-resolution IR radiometer||139,235
|-
|'''Santa Barbara Research Center'''||Medium-resolution IR||343,426
|-
|'''New Mexico College of Agriculture and Mechanic Arts'''||Antennas||69,384
|-
|'''California Computer Products, Inc.'''||Clock||{{N/A}}
|-
|'''[[Company:Ampex|Ampex]]'''||Tape recorder||{{N/A}}
|-
|'''Radiation Inc.'''||PCM telemetry||{{N/A}}
|-
|colspan="3"|Contract sums are for research for development and delivery for first two Nimbus launchings
|}
At the time of its launch, the idea that intangible properties such as air pressure could be observed using a satellite orbiting hundreds of miles above the Earth was revolutionary.{{citation needed|date=December 2011}} With each Nimbus mission, scientists broadened their ability to collect atmospheric characteristics that improved [[Earth:Weather forecasting|weather forecasting]], including ocean and air temperatures, air pressure, and [[Earth:Cloud|cloud]]iness.  Beginning with the Nimbus 3 satellite in 1969, temperature information through the atmospheric column began to be retrieved by satellites from the eastern Atlantic and most of the Pacific Ocean, which led to significant forecast improvements.<ref>{{cite journal|journal=Mariners Weather Log|title=SIRS and the Improved Marine Weather Forecast|author=National Environmental Satellite Center|publisher=Environmental Science Services Administration|pages=12–15|volume=14|number=1|date=January 1970}}</ref> The global coverage provided by Nimbus satellites made accurate 3–5 day forecasts possible for the first time.{{citation needed|date=December 2011}}

The ability of the Nimbus satellites to detect electromagnetic energy in multiple [[Wavelength|wavelength]]s (multi-spectral data), in particular the [[Physics:Microwave|microwave]] region of the [[Physics:Electromagnetic spectrum|electromagnetic spectrum]], made it possible for scientists to look into the atmosphere and tell the difference between [[Physics:Water vapor|water vapor]] and liquid water in clouds.{{citation needed|date=December 2011}} In addition, they were able to measure atmospheric temperature even in the presence of clouds,{{citation needed|date=December 2011}} a capability that allowed scientists to take the temperature in the "warm core" of hurricanes.{{citation needed|date=December 2011}}

===Radiation budget===
One of the most important scientific contributions of the Nimbus missions was their measurements of the Earth's radiation budget. For the first time, scientists had global, direct observations of the amount of solar radiation entering and exiting the Earth system. The observations helped to verify and refine the earliest climate models, and are still making important contributions to the study of [[Earth:Climate change|climate change]]. As scientists consider the causes and [[Biology:Effects of global warming|effects of global warming]], Nimbus radiation budget data provide a base for long-term analyses and make change-detection studies possible. The Nimbus technology gave rise to current radiation-budget sensors, such as the [[Astronomy:Clouds and the Earth's Radiant Energy System|CERES]] instruments on NASA's [[Engineering:Terra (satellite)|Terra]] and [[Engineering:Aqua (satellite)|Aqua]] satellites.<ref>{{cite web|title=The Earth's Radiation Budget|date=July 19, 2005 |url=https://earthobservatory.nasa.gov/Features/Nimbus/nimbus2.php|access-date=30 October 2017}}</ref>

===Ozone layer===
Even before the Nimbus satellites began collecting their observations of Earth's [[Physics:Ozone layer|ozone layer]], scientists had some understanding of the processes that maintained or destroyed it. They were pretty sure{{citation needed|date=December 2011}} they understood how the layer formed, and they knew from laboratory experiments that [[Chemistry:Halogen|halogen]]s could destroy [[Chemistry:Ozone|ozone]]. Finally, [[Earth:Weather balloon|weather balloon]]s had revealed that the concentration of ozone in the atmosphere changed over time, and scientists suspected weather phenomena or seasonal change were responsible. But how all of these pieces of information worked together on a global scale was still unclear.{{citation needed|date=December 2011}}

Scientists conducted experiments from NASA experimental aircraft and proved that atmospheric chemicals such as the [[Earth:Chlorofluorocarbon|chlorofluorocarbon]]s (CFCs) released from [[Chemistry:Refrigerant|refrigerant]]s and aerosol sprays did destroy ozone. As Nimbus 7 satellite observations accumulated between 1978 and 1994, it became increasingly clear that CFCs were creating an ozone hole each winter season over [[Earth:Antarctica|Antarctica]]. Not only that, but despite some year-to-year variations, it appeared the hole was becoming larger. The Nimbus measurements made clear how severe the ozone hole problem was.<ref name="Bhartia McPeters 2018 pp. 335–340">{{cite journal | last1=Bhartia | first1=Pawan Kumar | last2=McPeters | first2=Richard D. | title=The discovery of the Antarctic Ozone Hole | journal=Comptes Rendus Geoscience | publisher=Elsevier BV | volume=350 | issue=7 | year=2018 | issn=1631-0713 | doi=10.1016/j.crte.2018.04.006 | pages=335–340| bibcode=2018CRGeo.350..335B | doi-access=free | hdl=2060/20190002263 | hdl-access=free }}</ref>

===Sea ice===
Nimbus satellites collected orbital data on the extent of the polar caps in the mid-1960s, recorded in the visible and infrared parts of the spectrum. These first global snapshots of Earth's icecaps provide invaluable reference points for climate change studies. During a narrowing window of opportunity for [[Data archaeology|data archaeology]], the [[Organization:National Snow and Ice Data Center|National Snow and Ice Data Center]] (NDISC) and NASA were able to recover data that allowed the reconstruction of high-resolution Nimbus 2 images from 1966 showing the entire Arctic and Antarctic ice caps.<ref>[http://nsidc.org/monthlyhighlights/2010/02/techno-archaeology-rescues-climate-data-from-early-satellites/ Techno-archaeology rescues climate data from early satellites] {{Webarchive|url=https://web.archive.org/web/20130113224016/http://nsidc.org/monthlyhighlights/2010/02/techno-archaeology-rescues-climate-data-from-early-satellites/ |date=January 13, 2013 }} U.S. National Snow and Ice Data Center (NSIDC), January 2010 [https://web.archive.org/web/20100926041936/http://nsidc.org/monthlyhighlights/january2010.html WebCitation Archive]</ref>

When the Nimbus 5 spacecraft launched in 1972, scientists planned for its Electrically Scanning Microwave Radiometer to collect global observations of where and how much it rained across the world. However, a new priority for the sensor evolved in the months following its launch: mapping global [[Earth:Sea ice|sea ice]] concentrations. When Nimbus 7 launched in 1978, technology had improved enough for scientists to distinguish newly formed (i.e., "first year") sea ice from older ice, with the Scanning Multichannel Microwave Radiometer (SMMR) sensor. The data it collected during its 9-year lifespan provide a significant chunk of the long-term record of Earth's [[Physics:Sea ice concentration|sea ice concentration]] that today's scientists use for studies of climate change.

Among the most serendipitous discoveries that the Nimbus missions made possible was that of a gaping hole in the sea ice around Antarctica in the Southern Hemisphere winters of 1974–76. In a phenomenon that has not been observed since, an enormous, ice-free patch of water, called a [[Earth:Polynya|polynya]], developed three years in a row in the seasonal ice that encases Antarctica each winter. Located in the Weddell Sea, each year the polynya vanished with the summer melt, but returned the following year. The open patch of water may have influenced ocean temperatures as far down as 2,500 meters and influenced ocean circulation over a wide area. The Weddell Sea Polynya has not been observed since the event witnessed by the Nimbus satellites in the mid-70s.

===Global positioning system===
Nimbus satellites (beginning with Nimbus 3 in 1969) blazed the trail into the modern [[Engineering:GPS|GPS]] era with operational search and rescue and data collection systems. The satellites tested the first technology that allowed satellites to locate weather-observation stations set up in remote locations and to command the stations to transmit their data back to the satellite. The most famous demonstration of the new technology was through the record-breaking flight of British aviator Sheila Scott, who tested the Nimbus navigation and locator communication system when she made the first-ever solo flight over the [[Earth:North Pole|North Pole]] in 1971.

The Nimbus ground-to-satellite-to-ground communication system demonstrated the first satellite-based search and rescue system. Among the earliest successes were the rescue of two [[Engineering:Hot air balloon|hot air balloon]]ists who went down in the North Atlantic in 1977 and, later that year, tracking a {{wipe|Japan}}ese adventurer on his first attempt to be the first person to dogsled solo to the North Pole through [[Place:Greenland|Greenland]]. Tens of thousands of people over the past three decades have been rescued through the Search and Rescue Satellite-aided Tracking (SARSAT) operational system on NOAA satellites.

===Nuclear power===
Nimbus-3 was the first satellite to use a SNAP-19 [[Physics:Radioisotope thermoelectric generator|radioisotope thermoelectric generator]] (RTG) in space. A previous attempt was made to launch a SNAP-19 RTG on Nimbus-B-1, but the rocket was destroyed and the nuclear fuel landed in the Santa Barbara Channel. Later, the fuel was recovered from the wreckage at a depth of {{convert|300|ft}} and re-purposed for Nimbus-3 as the SNAP-19B.<ref name="Atomic">{{cite web |title=Atomic Power in Space II: A History 2015 |url=https://www.inl.gov/wp-content/uploads/2014/10/AtomicPowerInSpaceII-AHistory_2015_Appendices-References1.pdf |website=inl.gov |publisher=Idaho National Laboratory |access-date=13 June 2018 |date=September 2015}}</ref> This power source augmented the solar array with an additional {{val|28.2|u=W}} of electrical power.<ref>{{cite web |title=Nimbus III – NASA Radioisotope Power Systems |url=https://rps.nasa.gov/missions/8/nimbus-iii/ |website=NASA Radioisotope Power Systems |publisher=NASA |access-date=15 June 2018}}</ref>

==Operation history of the Nimbus satellites==
{|class="wikitable" style="border: 1px solid #000; border-collapse: collapse;"
!Satellite!!Launch Date!!Decay Date!!Perigee!!Apogee!!Launch Site!!Launch Vehicle!!COSPAR ID!!Mass
|-
|[[Engineering:Nimbus 1|Nimbus 1]]||August 28, 1964||May 16, 1974||429&nbsp;km||937&nbsp;km||{{wipe|Vandenberg Air Force Base}}||[[Engineering:Thor-Agena|Thor-Agena]] B||1964-052A||374&nbsp;kg
|-
|[[Engineering:Nimbus 2|Nimbus 2]]||May 15, 1966<ref>{{cite journal|title=On the Editor's Desk|page=122|journal=Mariners Weather Log|author=Environmental Science Services Administration|publisher=Department of Commerce|date=July 1966|volume=10|number=4}}</ref>||January 17, 1969||1103&nbsp;km||1169&nbsp;km||{{wipe|Vandenberg Air Force Base}}||Thor-Agena B||1966-040A||413&nbsp;kg
|-
|[[Engineering:Nimbus B|Nimbus B]]||May 18, 1968<ref>[https://www.smithsonianmag.com/science-nature/day-nimbus-weather-satellie-180961686/#VSeWSGocqrSbQwRp.99 The Day the Nimbus Weather Satellite Exploded], by Maya Wei-Haas, ''Smithsonian'' magazine (January 2017)
</ref> ||Destroyed at launch||---||---||{{wipe|Vandenberg Air Force Base}}||Thor-Agena D||{{n/a}}||572&nbsp;kg 
|-
|[[Engineering:Nimbus 3|Nimbus 3]]||April 13, 1969||January 22, 1972||1075&nbsp;km||1135&nbsp;km||{{wipe|Vandenberg Air Force Base}}||Thor-Agena B||1969-037A||576&nbsp;kg
|-
|[[Engineering:Nimbus 4|Nimbus 4]]||April 8, 1970||September 30, 1980||1092&nbsp;km||1108&nbsp;km||Vandenberg SLC-2E||Thor-Agena||1970-025A||619&nbsp;kg
|-
|[[Engineering:Nimbus 5|Nimbus 5]]||December 11, 1972||{{center|-}}||1089&nbsp;km||1101&nbsp;km||Vandenberg SLC-2W||[[Engineering:Delta (rocket family)|Delta]]||1972-097A||770&nbsp;kg
|-
|[[Engineering:Nimbus 6|Nimbus 6]]||June 12, 1975||{{center|-}}||1093&nbsp;km||1101&nbsp;km||Vandenberg SLC-2W||Delta||1975-052A||585&nbsp;kg
|-
|[[Engineering:Nimbus 7|Nimbus 7]]||October 24, 1978||{{center|1994}}||941&nbsp;km||954&nbsp;km||Vandenberg SLC-2W||Delta||1978-098A||832&nbsp;kg
|}

==See also==
*Coastal Zone Color Scanner


==References==
{{Reflist}}

==External links==
*http://nssdc.gsfc.nasa.gov/earth/nimbus.html Nimbus Program
*http://nssdc.gsfc.nasa.gov/earth/nimbus_sensor.html Experimental Instrumentation on-board Nimbus satellites


[[Category:Weather satellites of the United States]]
[[Category:Satellite series]]
[[Category:NASA programs]]

{{Sourceattribution|Nimbus program}}