Mundo: Pagkakaiba sa mga binago
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dito muna ilagay sa depinisyon niya bilang mundo na katumbas ng world sa english wikipedia habang wala pang concensus. huwag munang i-revert. maglalagay ako ng bagong paksa sa kapihan para humingi ng consensus Tatak: Manual revert Reverted Disambiguation links |
Ang tanging consensus na tatanggapin ng mga estudyante ay consensus ng mga akadamiko at historiograpo at siyentipiko, Tatak: Undo Reverted Disambiguation links |
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{{About|Planeta|Other user|Mundo (paglilinaw)}}
{{Infobox planet
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This infobox has been formatted in the same way as those for other Solar System
planets and bodies, so please do not change it without discussion on the talk page.
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| background = #f8f9fa
| name = Earth
| alt_names = [[Gaia]], [[wikt:Terra|Terra]], [[Terra (mythology)|Tellus]], [[Daigdig]], [[Globo]]
| adjectives = Earthly, terrestrial, terran, tellurian
| symbol = [[File:Earth symbol (bold).svg|24px|🜨]]
| image = The Blue Marble (remastered).jpg
| image_alt = [[Timeline of first images of Earth from space|Photograph of Earth]], taken by the [[Apollo 17]] mission. The Arabian peninsula, Africa and Madagascar lie in the lower half of the disc, whereas Antarctica is at the top.
| caption = A [[Timeline of first images of Earth from space|photograph of Earth]] taken by the crew of [[Apollo 17]] in 1972. A processed version became widely known as ''[[The Blue Marble]]''.<ref name=Petsko>{{cite journal |title=The blue marble |journal=[[Genome Biology]] |last=Petsko |first=Gregory A. |author-link=Gregory Petsko|volume=12 |issue=4 |page=112 |date=28 April 2011 |doi=10.1186/gb-2011-12-4-112 |pmc=3218853 |pmid=21554751}}</ref><ref name="NASAmarble">{{cite web |url=https://spaceflight.nasa.gov/gallery/images/apollo/apollo17/html/as17-148-22727.html |title=Apollo Imagery – AS17-148-22727 |publisher=NASA |date=1 November 2012 |access-date=22 October 2020 |archive-date=20 April 2019 |archive-url=https://web.archive.org/web/20190420043021/https://spaceflight.nasa.gov/gallery/images/apollo/apollo17/html/as17-148-22727.html |url-status=dead}}</ref>
| epoch = [[J2000.0|J2000]]
| aphelion = {{convert|152,100,000|km|mi|comma=gaps|abbr=on|disp=x| <small>(|)</small>}}
| perihelion = {{convert|147,095,000|km|mi|comma=gaps|abbr=on|disp=x| <small>(|)</small>}}
| time_periastron = 2023-Jan-04<ref name=horizons-perihelion>{{Cite web|url=https://ssd.jpl.nasa.gov/horizons_batch.cgi?batch=1&COMMAND=%27399%27&START_TIME=%272023-01-01%27&STOP_TIME=%272023-01-10%27&STEP_SIZE=%271%20hour%27&QUANTITIES=%2720%27&CENTER=%27@Sun%27|title=HORIZONS Batch call for 2023 perihelion|website=ssd.jpl.nasa.gov|publisher=NASA/JPL|access-date=3 July 2022}}</ref>
| semimajor = {{convert|149,598,023|km|mi|comma=gaps|abbr=on|disp=x| <small>(|)</small>}}
| eccentricity = {{val|0.0167086}}
| period = {{convert|365.256363004|d|yr|comma=gaps|abbr=on|lk=out|disp=x|<br /><small>(|[[julian year (astronomy)|<sub>j</sub>]])</small>}}
| avg_speed = {{convert|29.78|km/s|km/h mph|comma=gaps|abbr=on|disp=x|<br /><small>(|)</small>}}
| mean_anomaly = {{val|358.617|u=°}}
| inclination = {{ublist|class=nowrap |{{val|7.155|u=°}} to the [[Sun]]'s equator; |{{val|1.57869|u=°}}to [[invariable plane]]; |{{val|0.00005|u=°}} to J2000 [[ecliptic]]}}
| asc_node = {{val|-11.26064|u=°}}to J2000 ecliptic
| arg_peri = {{val|114.20783|u=°}}
| satellites =
{{unbulleted list
| 1 natural satellite: the [[Moon]]
| 5 [[quasi-satellite]]s
| >4 500 operational [[artificial satellite]]s
| >18 000 tracked [[space debris]]
}}
| allsatellites = yes
| mean_radius = {{convert|6371.0|km|mi|comma=gaps|abbr=on|disp=x| <small>(|)</small>}}
| equatorial_radius = {{convert|6378.137|km|mi|comma=gaps|abbr=on|disp=x| <small>(|)</small>}}
| polar_radius = {{convert|6356.752|km|mi|comma=gaps|abbr=on|disp=x| <small>(|)</small>}}
| flattening = 1/{{val|298.257222101}} ([[ETRS89]])
| circumference =
{{unbulleted list |class=nowrap
| {{convert|40075.017|km|mi|comma=gaps|abbr=on|disp=x| <small>[[equator]]ial (|)</small>}}[[World Geodetic System]] (''WGS-84''). <ref>[http://earth-info.nga.mil/GandG/wgs84/ Available online] {{Webarchive|url=https://web.archive.org/web/20200311023739/https://earth-info.nga.mil/GandG/wgs84/ |date=11 March 2020 }} from [[National Geospatial-Intelligence Agency]].</ref>
| {{convert|40007.86|km|mi|comma=gaps|abbr=on|disp=x| <small>[[Meridian (geography)|meridional]] (|)</small>}}<ref group="n" name="circ">Earth's [[circumference]] is almost exactly 40,000 km because the meter was calibrated on this measurement—more specifically, 1/10-millionth of the distance between the poles and the equator.</ref>
}}
| surface_area =
{{unbulleted list |class=nowrap
| {{convert|510072000|km2|mi2|comma=gaps|abbr=on|disp=x| <small>(|)</small>}}
| {{convert|148940000|km2|mi2|comma=gaps|abbr=on|disp=x| land <small>(|)</small>}}
| {{convert|361132000|km2|mi2|comma=gaps|abbr=on|disp=x| ocean <small>(|)</small>}}
}}
| volume = {{val|1.08321|e=12|u=km3}} <small>({{val|2.59876|e=11|u=cu mi}})</small>
| mass = {{val|5.97217|e=24|u=kg}} <small>({{val|1.31668|e=25|u=lb}})</small> <br /> <small>({{val|3.0|e=-6|ul=solar mass}})</small>
| density = {{convert|5.514|g/cm3|lb/cuin|comma=gaps|abbr=on|disp=x| <small>(|)</small>}}
| surface_grav = {{convert|9.80665|m/s2|ft/s2|comma=gaps|abbr=on|disp=x| <small>([[Gravity of Earth|{{val|1|u=''g''}}]]; |)</small>}}
| moment_of_inertia_factor = 0.3307
| escape_velocity = {{convert|11.186|km/s|km/h mph|comma=gaps|abbr=on|disp=x| <small>(|)</small>}}
| rotation = {{longitem|{{val|1.0|u=d}} <br /> <small>(24h 00m 00s)</small>}}
| sidereal_day = {{longitem|{{val|0.99726968|u=d}}<br /> <small>(23h 56m 4.100s)</small>}}
| rot_velocity = {{convert|1674.4|km/h|km/s km/h mph|order=out|comma=gaps|abbr=on|disp=x| <br /> <small>(|)</small>}}
| axial_tilt = {{val|23.4392811|u=°}}
| albedo = {{ublist|class=nowrap |0.367 [[Geometric albedo|geometric]]|0.306 [[Bond albedo|Bond]]}}
| atmosphere = yes
| temp_name1 = Celsius
| min_temp_1 = −89.2 °C
| mean_temp_1 = 14 °C ''(1961–90)''<ref>{{cite journal |last1=Jones |first1=P. D. |author-link1=Phil Jones (climatologist)|last2=Harpham |first2=C. |title=Estimation of the absolute surface air temperature of the Earth |journal=Journal of Geophysical Research: Atmospheres |date=2013 |volume=118 |issue=8 |pages=3213–3217 |doi=10.1002/jgrd.50359 |bibcode=2013JGRD..118.3213J |language=en |issn=2169-8996|doi-access=free }}</ref>
| max_temp_1 = 56.7 °C
| temp_name2 = Fahrenheit
| min_temp_2 = −128.5 °F
| mean_temp_2 = 57 °F ''(1961–90)''
| max_temp_2 = 134.0 °F
| surface_equivalent_dose_rate = {{convert |2.40 |mSv/yr |μSv/h |disp=out}}<ref name="UNSCEAR2008">{{cite book |author=United Nations Scientific Committee on the Effects of Atomic Radiation |title=Sources and effects of ionizing radiation |date=2008 |publication-date=2010 |publisher=United Nations |location=New York |isbn=978-92-1-142274-0 |url=http://www.unscear.org/unscear/en/publications/2008_1.html |access-date=9 November 2012 |at=Table 1}}</ref>
| surface_pressure = {{val|101.325|ul=kPa}} (at [[Sea level|MSL]])
| atmosphere_composition =
{{unbulleted list |class=nowrap
| 78.08% [[nitrogen]] ({{chem2|N2}}; dry air)
| 20.95% [[oxygen]] ({{chem2|O2}})
| ~ 1% [[water vapor]] <small>([[climate]] variable)</small>
| 0.9340% [[argon]]
| 0.0413% [[carbon dioxide]]<ref name="NOAA">{{cite web |url=https://www.esrl.noaa.gov/gmd/ccgg/trends/gl_trend.html |title=Trends in Atmospheric Carbon Dioxide: Recent Global CO<sub>2</sub> Trend |publisher=[[National Oceanic and Atmospheric Administration]] |website=[[Earth System Research Laboratory]] |date=19 October 2020 |archive-url=https://web.archive.org/web/20201004010704/https://www.esrl.noaa.gov/gmd/ccgg/trends/gl_trend.html |archive-date=4 October 2020 |url-status=live}}</ref>
| 0.00182% [[neon]]
| 0.00052% [[helium]]
| 0.00019% [[methane]]
| 0.00011% [[krypton]]
| 0.00006% [[hydrogen]]
}}
| note = no
}}
{{Human timeline}}
{{Life timeline}}
Ang '''Planetang Mundo'''<ref>https://www.deped.gov.ph/2021/04/19/pinasiglang-mundo-deped-holds-earth-day-celebration/</ref><ref>https://www.nasa.gov/sites/default/files/atoms/files/smd_esd_tagalog_tagged.pdf</ref><ref>https://www.nasa.gov/sites/default/files/atoms/files/smd_apd_tagalog_tagged.pdf</ref> ang ikatlong [[planeta]] mula sa [[araw]](na isang [[bituin]] sa [[uniberso]]) sa [[Sistemang Solar]]. Bagaman, ang mga [[tubig]] ay matatagpuan rin sa ibang planeta, ang mundo ang tanging mayroong likidong tubig sa ibabaw nito. Ang 71% ng mundo ay binubuo ng [[karagatan]] at ang natitirang 29% ng mundo ay binubuo ng [[lupain]] na binubuo ng mga [[kontinente]] at mga [[kapuluan]]. Ang surpasyo sa ibabaw ng mundo ay nabuo ng dahan-dahan sa paggalawa ng [[tektonika ng plaka]] na sanhi ng mga pagkakabuo ng mga [[bundok]], mga [[bulkan]], at mga [[lindol]]. Ang likidong labasang core ng mundo ay lumilikha ng magnetikong field na humuhugis na [[magnetospero]] ng mundo at humaharang sa mga nakakawasak na [[hanging solar]]. Ang atmospero ng mundo ay binubuo ng halos [[nitroheno]] at [[oksiheno]]. Ang mas maraming enerhiya mula sa [[araw]] ay nakukuha ng mga rehiyong tropiko kesa sa mga rehiyon sa polo nito.Ang [[bapor ng tubig]] ay umiiral sa atmospero ng mundo at bumubuo ng mga [[ulap]] na tumatakip sa mundo. Ang mga [[gaas na greenhouse]] sa atmospero gaya ng [[karbon dioksido]] (CO<sub>2</sub>) ay bumibihag sa enerhiya mula sa araw na malapit sa surpasyo nito. Ang klima ng rehiyon ay pinangangasiwaan ng latitud at elebasyon at lapit sa sa mga karaagatan. Ang hugis ng mundo ay isang [[ellipsoid]] na may sirkumperensiyang 40,000 km. Ito ang pinakasiksik na planeta sa [[sistemang solar]]. Ito ang isa sa apat na mabatong mga planeta at ang pinakamalaki. Ang mundo ay mga 8 minuto malayo sa araw at umiinog dito sa loobg 365.25 araw upang bumuo ng isang rebolusyon. Ang mundo ay umiinog rin sa sarili nitong aksis sa sa loob ng 23 oras at 56 minuto. Ang rotasyon ng aksis ng mundo ay pahalang sa planong orbital nito sa araw na lumilikha ng mga panahon(season). Ang mundo ay iniinugan ng isnag natural na satellite na [[buwan]] sa 380,000 km (mga 1.3 segundo ng [[liwanag]]. Ang mundo ay nabuo noong 4.5 bilyong taon ang nakakalipas. Sa unang bilyong taon ng kasaysayan ng mundo, ang karagatan ay nabuo at ang unang [[buhay]] ay umunlad mula rito. Ang buhay ay kumalat sa buong mundo na umapekto sa atmospero nito at surpasyon na humantong sa [[Dakilang pangyayaring oksidasyon]] noong 2 bilyong taon ang nakakalpas. Ang mga ninuno ng modernong [[tao]] ay lumitaw noong mga 300,000 taong nakakalipas.
==Mga sanggunian==
{{reflist}}
<references group="n"/>
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