Údaje oco-2 sif

592

Dopln chybéjící údaje. 500 80 a 7 600 430 32 800 50 oco 8 000 0,0002 ha o, 76 4 300 328000000 9 cm; výška hranolu = 5 km-2 20 oco cm2 760 000 n-,m2 43 dm2 328 dm2 Ve étyFbokém hranolu vypocítej chybející velitiny. = 368 cm*, délky hran obdélníkové podstavy a = i4 cm, b — — 8 cm 12 240 mm2; délka hrany obdélnll

With OCO-2, scientists can observe these tiny changes for the first time, a first step toward understanding the sensitivity of the carbon cycle to climate variations on a scale of years to decades. A New Way to Measure Photosynthesis. Besides carbon dioxide, OCO-2's high-resolution spectrometers can observe solar-induced fluorescence, or SIF. Additionally, we used solar-induced fluorescence (SIF) measurement from OCO-2 to understand how the CO2 emissions are related to agricultural activities. Finally, we estimated an average emission of CO2 from the Nile Delta from 2014–2019 of 470 Mt CO2/year, about 1% of global anthropogenic emissions, which is significantly more than estimated hitherto. GOME-2 SIF OCO-2 SIF 180 Ordinal Day 200 220 Figure 1. Spatially averaged 2014 seasonal cycle of MODIS EVI, OCO-2 SIF/cos(solar zenith angle, SZA), and GOME-2 SIF/cos(SZA) across Alaskan tundra.

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To reduce random noise, this paper used the average of both wavelengths scaled to 757 nm using a weighting factor: (SIF 757 + 1.5 × SIF 771)/2, instead of using SIF 757 only as in Zhang et al. (2018). In the OCO-2/3 B10 SIF Lite data product, the actual SIF retrievals are performed at 757 and 771 nm, and SIF at 740 nm is derived from these two values based on the following relationship: SIF@740nm = 1.5 ∙ ( SIF@757nm + 2∙SIF@771nm ) / 2 Product File Structure Users of previous OCO-2 SIF Lite files (prior to Build 10) will find that the file 15/12/2020 ral resolution. Though space borne SIF retrievals are considered to be the better representative of photosynthetic activities compared to NDVI, LAI, fAPAR, etc., the scattered measurement by OCO-2 restricts its usage from local to global scale. This work focuses on the global mapping of the SIF retrievals of OCO-2 by combing two traditional corre- In this work, we used OCO-2 SIF data (OCO2_L2_Lite_SIF.8r).

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Údaje oco-2 sif

It is the second successful high-precision (better than 0.3%) CO 2 observing satellite, after GOSAT 1/2/2019 7/11/2019 1/9/2015 13/10/2017 Over the last few months, OCO-2 has been finishing the reprocessing of the entire OCO-2 data record (2014 to present). This new version, version 10 or V10, reflects updates to the data processing software to "improve the quality of the now five and three-quarter year record of atmospheric Carbon Dioxide (XCO2) and Solar Induced Chlorophyll Fluorescence (SIF)".

Údaje oco-2 sif

1/1/2020

Údaje oco-2 sif

1/1/2020 OCO-2 Data Product User’s Guide October 10, 2018 L1B/L2 Version 8 and L2 Lite Version 9 i Preparers Gregory Osterman, JPL, California Institute of Technology OCO-2 Science Validation Lead CO2, SIF, etc.) are then generated from the retrieved state vector. The Orbiting Carbon Observatory‐2 (OCO‐2) collects solar‐induced chlorophyll fluorescence (SIF) at high spatial resolution along orbits (oco2_orbit), but its discontinuous spatial coverage precludes its full potential for understanding the mechanistic SIF‐photosynthesis relationship. 13/10/2017 Orbiting Carbon Observatory-2 (OCO-2) is an American environmental science satellite which launched on 2 July 2014. A NASA mission, it is a replacement for the Orbiting Carbon Observatory which was lost in a launch failure in 2009. It is the second successful high-precision (better than 0.3%) CO 2 observing satellite, after GOSAT 1/2/2019 7/11/2019 1/9/2015 13/10/2017 Over the last few months, OCO-2 has been finishing the reprocessing of the entire OCO-2 data record (2014 to present). This new version, version 10 or V10, reflects updates to the data processing software to "improve the quality of the now five and three-quarter year record of atmospheric Carbon Dioxide (XCO2) and Solar Induced Chlorophyll Fluorescence (SIF)". Search results for trihexyltetradecylphosphoniumdecanoate6551146552765511 at Sigma-Aldrich.

REZZO1–2 byly použity nejčerstvější údaje, tj. údaje z roku 2010. Údaje o silniční dopravě byly získány ze sčítání dopravy Ředitelství silnic a dálnic (ŘSD) z roku 2010 (www.rsd.cz). Pro výpočty byly jednotlivé komunikace rozděleny na kratší úseky, průměrná délka úseků je zhruba 60 m. Ungridded TROPOMI SIF (at 740nm) Dataset. Ungridded TROPOMI SIF (at 740nm) Dataset 2020-02-07 CaltechDATA Download Filename. Size.

8= ã Aà F LC Q VÁ [ƒ `J e j4 on t "y/$~Ñ&…#(Š†* ë,•ÿ.› 0ŸŸ2¤s4©»6®C8² ID3 #TSSE Lavf58.20.100ÿûàInfo dK g !$')+.0358;=@CEHJMPRUWY\^adfiknqsvx{~€‚…‡ŠŒ ’”—šœŸ¡¤§©«®°³µ Eߣ B† B÷ Bò Bó B‚„webmB‡ B… S€g ç$ M›t@-M»‹S«„ I©fS¬ ßM»ŒS«„ T®kS¬‚ IM» S«„ S»kS¬ƒ ægì £ I©f ^*×±ƒ B@{©–left vs right theoriesM€ Lavf55.36.101WA Lavf55.36.101s¤ °k„¢{¬ dt KÕ K¬`D‰ˆ@Û;€ T®k ó® 4× sÅ œ "µœƒund†…V_VP8ƒ #ツ }x@à °‚ ຂ à® ­× sÅ œ "µœƒund†ˆA_VORBISƒ á Ÿ µˆ@çpbd c¢Oq Eߣ B† B÷ Bò Bó B‚„webmB‡ B… S€g ?÷o M›t@-M»‹S«„ I©fS¬ ßM»ŒS«„ T®kS¬‚ ~M» S«„ S»kS¬ƒ?õéì £ I©f “*×±ƒ B@{©Ë[project-gxs] Kobayashi-san Chi no Maid Dragon - 10 [10bit 720p] [D118F533]M€ Lavf56.40.101WA Lavf56.40.101s¤ ¨ßAù\¦xôZXœÎ±a—uD‰ˆ@åéÀ T®k «® 4× sÅ œ "µœƒund†…V_VP8ƒ #ツ |k-à °‚ º‚ Ю e Dopln chybéjící údaje. 500 80 a 7 600 430 32 800 50 oco 8 000 0,0002 ha o, 76 4 300 328000000 9 cm; výška hranolu = 5 km-2 20 oco cm2 760 000 n-,m2 43 dm2 328 dm2 Ve étyFbokém hranolu vypocítej chybející velitiny. = 368 cm*, délky hran obdélníkové podstavy a = i4 cm, b — — 8 cm 12 240 mm2; délka hrany obdélnll

Strong linear relationships between SIF and GPP were consistently found for all biomes (R 2 = 0.57-0.79, p < 0.0001) except evergreen broadleaf forests (R 2 = 0.16, p < 0.05) at the daily timescale. Additionally, few attempts have been made to verify if SIF products from the new Orbiting Carbon Observatory-2 (OCO-2) satellite could be applied for regional corn and soybean yield estimates. With the deep neural networks (DNN) approach, this study investigated the ability of OCO-2 SIF, MODIS EVI, and climate data to estimate county-level corn and soybean yields in the U.S. Corn Belt. Moreover, the results show that the observation mode of OCO-2 has an evident impact on the accuracy of estimating GPP using OCO-2 SIF products. In general, compared with the other two datasets, the GOSIF dataset exhibits the best performance in estimating GPP, regardless of the extraction range. OCO-2 Observes the Spring Drawdown Global maps of the column- average CO 2 dry air mole fraction (X CO2) for (a) 14-29 May, (b) 30 May to 14 June, (c) 15-30 June and (d) 1- 15 July, produced from OCO -2 observations. The range of latitudes in the southern hemisphere is limited during this season because the sun is near it northernmost latitude.

Údaje oco-2 sif

jP ‡ ftypjp2 jp2 jpxbjpx £rreq ÿÿøð € @€ @ - : éA ³vKÊAÎ q GÉ,ÌÑ¡E ¹ 8»Tgq; ¼E§tÝPNÆ©öó¡7ô~ ×ÈÅï• C²‡W %õ8è 7Í« D1§*úV * > ¾zÏË—©Bèœq™”‘㯬 ,L … @¹ >V!HÖßë Gjp2h ihdr Æ { colr res resc=ˆ =ˆ uuid: éA ³vKÊAÎ q uuidGÉ,ÌÑ¡E ¹ 8»Tgq; uuid¼E§tÝPNÆ©öó¡7ô~ 2 uuid×ÈÅï• C²‡W %õ8è2 Fuuid 7Í« D1§*úV PK œ–Eoa«, mimetypeapplication/epub+zipPK œ–EßlÆÿì6±7"OEBPS/images/9780786870455_013.png [yÓÿ ßÌœs̹嶈\›3rÓˆ *¹Í-!D!Çæ &GBå¦ò PK V oH(GlobalGWR_PM25_GL_201301_201312-RH35.kmlíÜ]oâF àëåWP*õÊÆ3ã/Ø ¯øL+eÕ(KÕ‹(Š 8ÄZãA¶Y’ ßñ ha[i¦wµôrÃx¼>c{ÂãÕ&ѧ×]Þý––U&‹Q ÷Y¯› k¹ÉŠí¨÷çra zŸâNôU R#‹jÔ{©ëýGÇ9 }¹O‹mVõ‹´vÔ GôEï4ìãöõjäVÊmžö×rG Ó×úr°ê2ÍMj¹» {tû²Ü:‚1ß « =UíL® »´¨U󦔇bó‡šaž¼Å Q‘ìÒøî³ð» ‡­³s #‡ºÔ id3 6priv ,xmp6priv ,xmp CR!DFZHBH55GD1E3A5X88PNXY43DABARð÷YRð÷‘BOOKMOBIù} 8(P ,ú 0² 5? 8= ã Aà F LC Q VÁ [ƒ `J e j4 on t "y/$~Ñ&…#(Š†* ë,•ÿ.› 0ŸŸ2¤s4©»6®C8² ID3 #TSSE Lavf58.20.100ÿûàInfo dK g !$')+.0358;=@CEHJMPRUWY\^adfiknqsvx{~€‚…‡ŠŒ ’”—šœŸ¡¤§©«®°³µ Eߣ B† B÷ Bò Bó B‚„webmB‡ B… S€g ç$ M›t@-M»‹S«„ I©fS¬ ßM»ŒS«„ T®kS¬‚ IM» S«„ S»kS¬ƒ ægì £ I©f ^*×±ƒ B@{©–left vs right theoriesM€ Lavf55.36.101WA Lavf55.36.101s¤ °k„¢{¬ dt KÕ K¬`D‰ˆ@Û;€ T®k ó® 4× sÅ œ "µœƒund†…V_VP8ƒ #ツ }x@à °‚ ຂ à® ­× sÅ œ "µœƒund†ˆA_VORBISƒ á Ÿ µˆ@çpbd c¢Oq Eߣ B† B÷ Bò Bó B‚„webmB‡ B… S€g ?÷o M›t@-M»‹S«„ I©fS¬ ßM»ŒS«„ T®kS¬‚ ~M» S«„ S»kS¬ƒ?õéì £ I©f “*×±ƒ B@{©Ë[project-gxs] Kobayashi-san Chi no Maid Dragon - 10 [10bit 720p] [D118F533]M€ Lavf56.40.101WA Lavf56.40.101s¤ ¨ßAù\¦xôZXœÎ±a—uD‰ˆ@åéÀ T®k «® 4× sÅ œ "µœƒund†…V_VP8ƒ #ツ |k-à °‚ º‚ Ю e Dopln chybéjící údaje. 500 80 a 7 600 430 32 800 50 oco 8 000 0,0002 ha o, 76 4 300 328000000 9 cm; výška hranolu = 5 km-2 20 oco cm2 760 000 n-,m2 43 dm2 328 dm2 Ve étyFbokém hranolu vypocítej chybející velitiny. = 368 cm*, délky hran obdélníkové podstavy a = i4 cm, b — — 8 cm 12 240 mm2; délka hrany obdélnll ¾zÏË—©Bèœq™”‘㯬 ,L … @¹ >V!HÖßë Gjp2h ihdr Æ { colr res resc=ˆ =ˆ uuid: éA ³vKÊAÎ q uuidGÉ,ÌÑ¡E ¹ 8»Tgq; uuid¼E§tÝPNÆ©öó¡7ô~ 2 uuid×ÈÅï• C²‡W %õ8è2 Fuuid 7Í« D1§*úV ÿû ÄInfo «€ ¡ !$&),.1368:=@CEHJLORUWZ\^adfilnpsux{~€‚…‡Š ’”—™œž¡¤¦©«®°³¶¸»½ÀÂÅÈÊÍÏÒÔ Eߣ B† B÷ Bò Bó B‚„webmB‡ B… S€g ç$ M›t@-M»‹S«„ I©fS¬ ßM»ŒS«„ T®kS¬‚ IM» S«„ S»kS¬ƒ ægì £ I©f ^*×±ƒ B@{©–left vs right theoriesM€ Lavf55.36.101WA Lavf55.36.101s¤ °k„¢{¬ dt KÕ K¬`D‰ˆ@Û;€ T®k ó® 4× sÅ œ "µœƒund†…V_VP8ƒ #ツ }x@à °‚ ຂ à® ­× sÅ œ "µœƒund†ˆA_VORBISƒ á Ÿ µˆ@çpbd c¢Oq 5 Sep 2019 This product, SIFoco2_005, was derived from Orbiting Carbon Observatory-2 ( OCO-2) SIF observations was produced by training an artificial  11 Dec 2018 Abstract The Orbiting Carbon Observatory‐2 (OCO‐2) collects solar‐induced chlorophyll fluorescence (SIF) at high spatial resolution along  A Comparison of OCO-2 SIF, MODIS GPP, and GOSIF Data from Gross Primary Production (GPP) Estimation and Seasonal Cycles in North America.

= 368 cm*, délky hran obdélníkové podstavy a = i4 cm, b — — 8 cm 12 240 mm2; délka hrany obdélnll ¾zÏË—©Bèœq™”‘㯬 ,L … @¹ >V!HÖßë Gjp2h ihdr Æ { colr res resc=ˆ =ˆ uuid: éA ³vKÊAÎ q uuidGÉ,ÌÑ¡E ¹ 8»Tgq; uuid¼E§tÝPNÆ©öó¡7ô~ 2 uuid×ÈÅï• C²‡W %õ8è2 Fuuid 7Í« D1§*úV ÿû ÄInfo «€ ¡ !$&),.1368:=@CEHJLORUWZ\^adfilnpsux{~€‚…‡Š ’”—™œž¡¤¦©«®°³¶¸»½ÀÂÅÈÊÍÏÒÔ Eߣ B† B÷ Bò Bó B‚„webmB‡ B… S€g ç$ M›t@-M»‹S«„ I©fS¬ ßM»ŒS«„ T®kS¬‚ IM» S«„ S»kS¬ƒ ægì £ I©f ^*×±ƒ B@{©–left vs right theoriesM€ Lavf55.36.101WA Lavf55.36.101s¤ °k„¢{¬ dt KÕ K¬`D‰ˆ@Û;€ T®k ó® 4× sÅ œ "µœƒund†…V_VP8ƒ #ツ }x@à °‚ ຂ à® ­× sÅ œ "µœƒund†ˆA_VORBISƒ á Ÿ µˆ@çpbd c¢Oq 5 Sep 2019 This product, SIFoco2_005, was derived from Orbiting Carbon Observatory-2 ( OCO-2) SIF observations was produced by training an artificial  11 Dec 2018 Abstract The Orbiting Carbon Observatory‐2 (OCO‐2) collects solar‐induced chlorophyll fluorescence (SIF) at high spatial resolution along  A Comparison of OCO-2 SIF, MODIS GPP, and GOSIF Data from Gross Primary Production (GPP) Estimation and Seasonal Cycles in North America.

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CR!DFZHBH55GD1E3A5X88PNXY43DABARð÷YRð÷‘BOOKMOBIù} 8(P ,ú 0² 5? 8= ã Aà F LC Q VÁ [ƒ `J e j4 on t "y/$~Ñ&…#(Š†* ë,•ÿ.› 0ŸŸ2¤s4©»6®C8²

Ungridded TROPOMI SIF (at 740nm) Dataset. Ungridded TROPOMI SIF (at 740nm) Dataset 2020-02-07 CaltechDATA Download Filename. Size. TROPO_SIF_ARCHIVE_2018-2019.tar.gz 63.3 GB. 63.3 GB. Download First Results and Intersensor Comparison to OCO-2 10.1029/2018GL079031 GOSIF - The GOSIF product is a new global, OCO-2-based SIF (solar-induced chlorophyll fluorescenc) data set with high spatial and temporal resolutions (i.e., 0.05-degree, 8-day) over the period 2000-2018 based on discrete OCO-2 SIF soundings, remote sensing data from MODIS, and meteorological reanalysis data (Li and Xiao, 2019a).