WFRF:(Nassar R.)
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| Fältnamn | Indikatorer | Metadata |
|---|---|---|
| 000 | 03627naa a2200457 4500 | |
| 001 | oai:research.chalmers.se:69c18f43-f162-4184-9017-018230be8591 | |
| 003 | SwePub | |
| 008 | 171007s2006 | |||||||||||000 ||eng| | |
| 024 | 7 | a https://research.chalmers.se/publication/1028082 URI |
| 024 | 7 | a https://doi.org/10.1029/2006JD0070732 DOI |
| 040 | a (SwePub)cth | |
| 041 | a engb eng | |
| 042 | 9 SwePub | |
| 072 | 7 | a art2 swepub-publicationtype |
| 072 | 7 | a ref2 swepub-contenttype |
| 100 | 1 | a Nassar, R.u Harvard University,University of Waterloo4 aut |
| 245 | 1 0 | a A global inventory of stratospheric chlorine in 2004 |
| 264 | 1 | c 2006 |
| 520 | a Total chlorine (CITOT) in the stratosphere has been determined using the Atmospheric Chemistry Experiment Fourier Transform Spectrometer (ACE-FTS) measurements of HCl, ClONO2, CH3Cl, CCl4, CCl3F (CFC-11), CCl2F2 (CFC-12), CHClF2 (HCFC-22), CCl2FCClF2 (CFC-113), CH3CClF2 (HCFC-142b), COClF, and ClO supplemented by data from several other sources, including both measurements and models. Separate chlorine inventories were carried out in five latitude zones (60°-82°N, 30°-60°N, 30°S-30°N, 30°-60°S, and 60°-82°S), averaging the period of February 2004 to January 2005 inclusive, when possible, to deal with seasonal variations. The effect of diurnal variation was avoided by only using measurements taken at local sunset. Mean stratospheric ClTOT values of 3.65 ppbv were determined for both the northern and southern midlatitudes (with an estimated 1σ, accuracy of ±0.13 ppbv and a precision of ±.09 ppbv), accompanied by a slightly lower value in the tropics and slightly higher values at high latitudes. Stratospheric ClTOT profiles in all five latitude zones are nearly linear with a slight positive slope in ppbv /km. Both the observed slopes and pattern of latitudinal variation can be interpreted as evidence of the beginning of a decline in global stratospheric chlorine, which is qualitatively consistent with the mean stratospheric circulation pattern and time lag necessary for transport. | |
| 650 | 7 | a TEKNIK OCH TEKNOLOGIERx Maskinteknikx Rymd- och flygteknik0 (SwePub)203022 hsv//swe |
| 650 | 7 | a ENGINEERING AND TECHNOLOGYx Mechanical Engineeringx Aerospace Engineering0 (SwePub)203022 hsv//eng |
| 700 | 1 | a Bernath, P. F.u University of Waterloo4 aut |
| 700 | 1 | a Boone, C. D.u University of Waterloo4 aut |
| 700 | 1 | a Clerbaux, C.u Université libre de Bruxelles (ULB)4 aut |
| 700 | 1 | a Coheur, P. F.u Université libre de Bruxelles (ULB)4 aut |
| 700 | 1 | a Dufour, G.u Université Paris-Saclay,University Paris-Saclay4 aut |
| 700 | 1 | a Froidevaux, L.4 aut |
| 700 | 1 | a Mahieu, E.u Universite de Liège,University of Liège4 aut |
| 700 | 1 | a McConnell, J. C.u York University4 aut |
| 700 | 1 | a McLeod, S. D.u University of Waterloo4 aut |
| 700 | 1 | a Murtagh, Donal,d 1959u Chalmers tekniska högskola,Chalmers University of Technology4 aut0 (Swepub:cth)donal |
| 700 | 1 | a Rinsland, C. P.u NASA Langley Research Center4 aut |
| 700 | 1 | a Semeniuk, K.u York University4 aut |
| 700 | 1 | a Skelton, R.u University of Waterloo4 aut |
| 700 | 1 | a Walker, K. A.u University of Toronto,University of Waterloo4 aut |
| 700 | 1 | a Zander, R.u Universite de Liège,University of Liège4 aut |
| 710 | 2 | a Harvard Universityb University of Waterloo4 org |
| 773 | 0 | t Journal of Geophysical Researchg 111:22q 111:22x 0148-0227x 2156-2202 |
| 856 | 4 | u http://dx.doi.org/10.1029/2006JD007073y FULLTEXT |
| 856 | 4 8 | u https://research.chalmers.se/publication/102808 |
| 856 | 4 8 | u https://doi.org/10.1029/2006JD007073 |
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