Knowledge (XXG)

MOPITT

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In the two optical systems referred to above, eight channels measure carbon monoxide or methane. Channels one, two, three, five, six, and seven focus on carbon monoxide. The six channels for carbon monoxide vary in cell pressures from 25 to 800 mb, and their cell lengths range from 2 to 10 mm. Their
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coolers chill the dewar. Considerable heat-emitting units like the cooler are placed intentionally on the coldplate, and other critical electronic pieces are placed near it as well. The coldplate, located under MOPITT's baseplate, provides a stable thermal environment for the instrument. It utilizes
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Before MOPITT's release, data on carbon monoxide was limited. With MOPITT's comprehensive measurements of carbon monoxide throughout the past two decades, scientists are better equipped to predict the potential consequences of carbon monoxide pollution. Its applications include:
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in 4.6-μm absorption. MOPITT can view different layers of the troposphere by varying modulated cells: Pressure-modulated cells (PMCs) are used to observe upper layers while length-modulated cells (LMCs) can view lower layers of the troposphere.
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on December 18, 1999, and began scientific measurements in March 2000. Before its execution, the only existing global carbon monoxide dataset was measured by the MAPS instrument aboard space shuttles. MOPITT is the first tool to measure global
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These channels absorb different amounts of energy, leading to differences in the resulting signals that correlate to the spectral sample of carbon monoxide. To further analyze carbon monoxide levels, MOPITT adjusts the path length or gaseous
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Kar, Jayanta; Bremer, Holger; Drummond, James R.; Rochon, Yves J.; Jones, Dylan B. A.; Nichitiu, Florian; Zou, Jason; Liu, Jane; Gille, John C.; Edwards, David P.; Deeter, Merritt N.; Francis, Gene; Ziskin, Dan; Warner, Juying (2004-12-16).
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Edwards, D. P.; Emmons, L. K.; Hauglustaine, D. A.; Chu, D. A.; Gille, J. C.; Kaufman, Y. J.; Pétron, G.; Yurganov, L. N.; Giglio, L.; Deeter, M. N.; Yudin, V.; Ziskin, D. C.; Warner, J.; Lamarque, J.-F.; Francis, G. L. (2004-12-27).
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Despite the initial five-year term plan, the satellite has continued to operate for over 20 years, and researchers expect all five of these instruments to maintain their functionality and transmit information and data past 2026.
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remote sensors on the Terra satellite, the spacecraft monitors the Earth's environment and climate changes. Following its construction in Canada, MOPITT was launched into Earth's orbit in 1999 and utilizes gas correlation
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also differs between channels, and the modulator types are either LMCs or PMCs. In contrast, channels four and eight measure methane, and their only difference is the different LMCs used. All channels operate at 300 K.
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holding the bulk of the apparatus. Results from the MOPITT enable scientists to better understand carbon monoxide's effects on a global scale, and various studies have been conducted based on MOPITT's measurements.
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to vary, which will give a difference and an average transmission. The difference specifies the gases measured, whereas the average signal indicates the overall radiation minus the initial gas measured.
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MOPITT's spatial resolution is 22 km horizontally and about 5 km vertically and scans Earth at a broad area of 640 km wide. The carbon monoxide measurement profiles are created through the upwelling of
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Drummond, James R.; Bailey, Paul L.; Brasseur, Guy; Davis, Gary R.; Gille, John C.; Peskett, Guy D.; Reichle, Henry K.; Roulet, N.; Mand, Gurpreet S.; Mcconnell, Jack C. (1999-10-01).
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Hedelius, Jacob K.; Toon, Geoffrey C.; Buchholz, Rebecca R.; Iraci, Laura T.; Podolske, James R.; Roehl, Coleen M.; Wennberg, Paul O.; Worden, Helen M.; Wunch, Debra (2021-03-16).
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Kar, Jayanta; Drummond, James R.; Jones, Dylan B. A.; Liu, Jane; Nichitiu, Florian; Zou, Jason; Gille, John C.; Edwards, David P.; Deeter, Merritt N. (August 2006).
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4.7 μm channels are referred to as the carbon monoxide thermal channels because the signals stem from the thermal emissions from Earth's surface and the atmosphere
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Clerbaux, Cathy; Edwards, David P.; Deeter, Merritt; Emmons, Louisa; Lamarque, Jean-François; Tie, Xue Xi; Massie, Steve T.; Gille, John (February 2008).
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or absorption between a known and unknown sample) to measure concentrations of carbon monoxide. Essentially, MOPITT takes carbon monoxide as an
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and variations in carbon monoxide. It is part of a series of five payloads on the Terra satellite that oversees global environmental changes:
692:"Large horizontal gradients in atmospheric CO at the synoptic scale as seen by spaceborne Measurements of Pollution in the Troposphere" 59:
to measure the presence of different gases in the troposphere. The fundamental operations occur in its optical system composed of two
739:"Southern Hemisphere carbon monoxide interannual variability observed by Terra/Measurement of Pollution in the Troposphere (MOPITT)" 174:
2.2 μm channels refer to the methane solar channels because reflected sunlight is the major signal, similar to the 2.3 μm channels
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The 2.3 μm channels are termed the carbon monoxide solar channel because they absorb the dominant signal from reflected sunlight
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Detection and analysis of carbon monoxide emitted by cities and urban areas to demonstrate rising carbon monoxide pollution
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Liu, J.; Drummond, J. R.; Jones, D. B. A.; Cao, Z.; Bremer, H.; Kar, J.; Zou, J.; Nichitiu, F.; Gille, J. C. (2006-01-27).
518:. SPIE's International Symposium on Optical Science, Engineering, and Instrumentation. Vol. 3756. pp. 396–402. 268: 81: 597:"Evidence of vertical transport of carbon monoxide from Measurements of Pollution in the Troposphere (MOPITT)" 937: 276:
Generating maps of pollution transport, such as the direction of carbon monoxide emissions after large fires
214: 786:"Carbon monoxide (CO) maximum over the Zagros mountains in the Middle East: Signature of mountain venting?" 349:"Measurements Of Pollution In The Troposphere (MOPITT) | Atmospheric Chemistry Observations & Modeling" 47: 645:"Observations of carbon monoxide and aerosols from the Terra satellite: Northern Hemisphere variability" 210: 77: 737:
Edwards, D. P.; Pétron, G.; Novelli, P. C.; Emmons, L. K.; Gille, J. C.; Drummond, J. R. (2006-08-27).
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At the heart of MOPITT lies the optical system, which is composed of two identical "mirror imaged"
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cooler assemblies containing cold optics and thermal and solar detectors. A pair of low-vibration
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founded the MOPITT project following its initial proposal in 1989. After the establishment of the
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The analysis of the variation in vertical structure of carbon monoxide caused by Asian summer
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MOPITT is a nadir-sounding (vertically downward pointing) instrument that measures upwelling
899: 852: 833:"Carbon monoxide pollution from cities and urban areas observed by the Terra/MOPITT mission" 805: 758: 711: 664: 616: 527: 316: 223: 942: 932: 895: 848: 801: 754: 707: 660: 612: 523: 513: 376: 880:"Regional and Urban Column CO Trends and Anomalies as Observed by MOPITT Over 16 Years" 309:
The observation of large horizontal gradients in carbon monoxide at the synoptic scale
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concentration in the troposphere allows scientists to perform interim pollution methods
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In the year 2022 alone, more than 250 studies have used measurements from MOPITT.
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Many studies utilizing MOPITT's data have been completed. Notable ones include:
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to measure the signal of the same gas in the troposphere. The sensor quantifies
43: 239: 147: 911: 864: 817: 770: 723: 676: 628: 545: 454: 903: 856: 809: 762: 715: 668: 620: 546:"Instrument Concepts | Atmospheric Chemistry Observations & Modeling" 180: 155: 139: 297: 227: 51: 531: 485: 455:"MOPITT - 20 Years of Measuring Atmospheric Pollution - CMOS Bulletin" 348: 312:
The study of carbon monoxide variability in the Southern Hemisphere
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Analysis of environmental pollution influenced by human activities
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Official website for MOPITT science and product development team
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Canadian scientific instrument aboard NASA's Terra satellite
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that portray areas producing or reducing carbon monoxide
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Breakdown of carbon monoxide trends in varying regions
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MOPITT instrument website at the University of Toronto
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that include the calibration sources, scan mirrors,
183:of the gas sample, causing the frequency of these 315:Observation of enhanced carbon monoxide over the 515:Early mission planning for the MOPITT instrument 158:emitted and reflected from Earth through three 114:(Moderate Resolution Imaging Spectroradiometer) 34:) is an ongoing astronomical instrument aboard 486:"Measurements Of Pollution In The Troposphere" 120:(Measurements of Pollution in the Troposphere) 102:(Clouds and the Earth's Radiant Energy System) 46:carbon monoxide levels. It is part of NASA's 8: 884:Journal of Geophysical Research: Atmospheres 743:Journal of Geophysical Research: Atmospheres 696:Journal of Geophysical Research: Atmospheres 649:Journal of Geophysical Research: Atmospheres 302:The examination of seasonal carbon monoxide 32:Measurements of Pollution in the Troposphere 943:MOPITT data available through NASA-Langley 256:A better understanding of the increase in 18: 337: 269:automobile emission reduction standards 108:(Multi-angle Imaging Spectroradiometer) 958:Atmospheric sounding satellite sensors 569:Agency, Canadian Space (2007-03-12). 480: 478: 476: 474: 7: 507: 505: 448: 446: 444: 370: 368: 343: 341: 142:radiation and utilizes correlation 50:(EOS), and combined with the other 23:MOPITT 2000 global carbon monoxide. 571:"Measuring atmospheric pollutants" 453:SCMO, CMOS Bulletin (2019-12-21). 14: 279:Confirmation of newly developed 74:National Research Council Canada 42:satellite that measures global 213:, LMCs, PMCs, modulators, and 1: 938:NASA WIST data archive system 837:Geophysical Research Letters 790:Geophysical Research Letters 601:Geophysical Research Letters 306:in the Northern Hemisphere 78:Canadian Space Agency (CSA) 974: 490:mopitt.physics.utoronto.ca 82:Vandenberg Air Force Base 201:Instrument Description 134:Instrument Methodology 48:Earth Observing System 24: 575:Canadian Space Agency 22: 904:10.1029/2020JD033967 857:10.1029/2007GL032300 810:10.1029/2006GL026231 763:10.1029/2006JD007079 716:10.1029/2005JD006076 669:10.1029/2004JD004727 621:10.1029/2004GL021128 896:2021JGRD..12633967H 849:2008GeoRL..35.3817C 802:2006GeoRL..3315819K 755:2006JGRD..11116303E 708:2006JGRD..111.2306L 661:2004JGRD..10924202E 613:2004GeoRL..3123105K 524:1999SPIE.3756..396D 401:"Terra (satellite)" 550:www2.acom.ucar.edu 459:CMOS BULLETIN SCMO 429:asdc.larc.nasa.gov 425:"ASDC | MOP03JM_8" 353:www2.acom.ucar.edu 267:practices such as 25: 532:10.1117/12.366395 965: 916: 915: 875: 869: 868: 828: 822: 821: 781: 775: 774: 734: 728: 727: 687: 681: 680: 639: 633: 632: 591: 585: 584: 582: 581: 566: 560: 559: 557: 556: 542: 536: 535: 509: 500: 499: 497: 496: 482: 469: 468: 466: 465: 450: 439: 438: 436: 435: 421: 415: 414: 413: 412: 397: 391: 390: 388: 387: 377:"MOPITT | Terra" 372: 363: 362: 360: 359: 345: 317:Zagros Mountains 224:capillary action 194:thermal radiance 973: 972: 968: 967: 966: 964: 963: 962: 948: 947: 924: 919: 877: 876: 872: 830: 829: 825: 783: 782: 778: 736: 735: 731: 689: 688: 684: 641: 640: 636: 593: 592: 588: 579: 577: 568: 567: 563: 554: 552: 544: 543: 539: 511: 510: 503: 494: 492: 484: 483: 472: 463: 461: 452: 451: 442: 433: 431: 423: 422: 418: 410: 408: 405:Knowledge (XXG) 399: 398: 394: 385: 383: 375:Thome, Kurtis. 374: 373: 366: 357: 355: 347: 346: 339: 335: 290: 249: 203: 146:(comparison of 136: 131: 70: 17: 12: 11: 5: 971: 969: 961: 960: 950: 949: 946: 945: 940: 935: 930: 923: 922:External links 920: 918: 917: 870: 823: 776: 729: 682: 634: 586: 561: 537: 501: 470: 440: 416: 392: 381:terra.nasa.gov 364: 336: 334: 331: 327: 326: 323: 320: 313: 310: 307: 300: 289: 286: 285: 284: 281:climate models 277: 274: 271: 263:Assessment of 261: 248: 245: 219:Stirling Cycle 207:optical tables 202: 199: 185:spectral lines 176: 175: 171: 170: 167: 160:spectral bands 152:optical filter 135: 132: 130: 127: 122: 121: 115: 109: 103: 97: 87:concentrations 69: 66: 61:optical tables 15: 13: 10: 9: 6: 4: 3: 2: 970: 959: 956: 955: 953: 944: 941: 939: 936: 934: 931: 929: 926: 925: 921: 913: 909: 905: 901: 897: 893: 889: 885: 881: 874: 871: 866: 862: 858: 854: 850: 846: 842: 838: 834: 827: 824: 819: 815: 811: 807: 803: 799: 795: 791: 787: 780: 777: 772: 768: 764: 760: 756: 752: 748: 744: 740: 733: 730: 725: 721: 717: 713: 709: 705: 701: 697: 693: 686: 683: 678: 674: 670: 666: 662: 658: 654: 650: 646: 638: 635: 630: 626: 622: 618: 614: 610: 606: 602: 598: 590: 587: 576: 572: 565: 562: 551: 547: 541: 538: 533: 529: 525: 521: 517: 516: 508: 506: 502: 491: 487: 481: 479: 477: 475: 471: 460: 456: 449: 447: 445: 441: 430: 426: 420: 417: 406: 402: 396: 393: 382: 378: 371: 369: 365: 354: 350: 344: 342: 338: 332: 330: 324: 321: 318: 314: 311: 308: 305: 301: 299: 295: 294: 293: 287: 282: 278: 275: 272: 270: 266: 265:antipollution 262: 259: 255: 254: 253: 246: 244: 241: 235: 233: 232:working fluid 229: 225: 220: 216: 212: 208: 200: 198: 195: 189: 186: 182: 173: 172: 168: 165: 164: 163: 161: 157: 153: 149: 145: 141: 133: 128: 126: 119: 116: 113: 110: 107: 104: 101: 98: 95: 92: 91: 90: 88: 83: 79: 75: 67: 65: 62: 58: 53: 49: 45: 41: 37: 33: 29: 21: 887: 883: 873: 840: 836: 826: 793: 789: 779: 746: 742: 732: 699: 695: 685: 652: 648: 637: 604: 600: 589: 578:. 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Retrieved 352: 328: 291: 250: 247:Applications 236: 204: 190: 177: 144:spectroscopy 137: 123: 117: 71: 57:spectroscopy 44:tropospheric 31: 27: 26: 304:climatology 148:wavelengths 580:2023-10-24 555:2023-11-07 495:2023-10-24 464:2023-10-24 434:2023-10-24 411:2023-10-24 386:2023-10-24 358:2023-10-24 333:References 240:wavelength 129:Technology 68:Background 912:2169-897X 865:0094-8276 818:0094-8276 771:0148-0227 724:0148-0227 677:0148-0227 629:0094-8276 952:Category 319:in Iran 298:monsoons 211:choppers 181:pressure 156:radiance 140:infrared 892:Bibcode 845:Bibcode 798:Bibcode 751:Bibcode 749:(D16). 704:Bibcode 657:Bibcode 655:(D24). 609:Bibcode 520:Bibcode 288:Studies 238:center 230:as its 228:ammonia 52:payload 910:  863:  816:  796:(15). 769:  722:  702:(D2). 675:  627:  607:(23). 118:MOPITT 28:MOPITT 890:(5). 843:(3). 258:ozone 226:with 215:dewar 112:MODIS 100:CERES 94:ASTER 40:Terra 908:ISSN 861:ISSN 814:ISSN 767:ISSN 720:ISSN 673:ISSN 625:ISSN 106:MISR 72:The 36:NASA 900:doi 888:126 853:doi 806:doi 759:doi 747:111 712:doi 700:111 665:doi 653:109 617:doi 528:doi 38:'s 954:: 906:. 898:. 886:. 882:. 859:. 851:. 841:35 839:. 835:. 812:. 804:. 794:33 792:. 788:. 765:. 757:. 745:. 741:. 718:. 710:. 698:. 694:. 671:. 663:. 651:. 647:. 623:. 615:. 605:31 603:. 599:. 573:. 548:. 526:. 504:^ 488:. 473:^ 457:. 443:^ 427:. 403:, 379:. 367:^ 351:. 340:^ 234:. 162:: 914:. 902:: 894:: 867:. 855:: 847:: 820:. 808:: 800:: 773:. 761:: 753:: 726:. 714:: 706:: 679:. 667:: 659:: 631:. 619:: 611:: 583:. 558:. 534:. 530:: 522:: 498:. 467:. 437:. 389:. 361:. 30:(

Index


NASA
Terra
tropospheric
Earth Observing System
payload
spectroscopy
optical tables
National Research Council Canada
Canadian Space Agency (CSA)
Vandenberg Air Force Base
concentrations
ASTER
CERES
MISR
MODIS
MOPITT
infrared
spectroscopy
wavelengths
optical filter
radiance
spectral bands
pressure
spectral lines
thermal radiance
optical tables
choppers
dewar
Stirling Cycle

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