• Nenhum resultado encontrado

[PDF] Top 20 Trends in stratospheric ozone derived from merged SAGE II and Odin-OSIRIS satellite observations

Has 10000 "Trends in stratospheric ozone derived from merged SAGE II and Odin-OSIRIS satellite observations" found on our website. Below are the top 20 most common "Trends in stratospheric ozone derived from merged SAGE II and Odin-OSIRIS satellite observations".

Trends in stratospheric ozone derived from merged SAGE II and Odin-OSIRIS satellite observations

Trends in stratospheric ozone derived from merged SAGE II and Odin-OSIRIS satellite observations

... Murtagh, D. P., Brohede, S., Stegman, J., Witt, G., Barnes, G., Payne, W. F., Piché, L., Smith, K., Warshaw, G., Deslauniers, D.-L., Marchand, P., Richardson, E. H., King, R. A., Wev- ers, I., McCreath, W., Kyrölä, E., ... See full document

28

Trends in stratospheric ozone derived from merged SAGE II and Odin-OSIRIS satellite observations

Trends in stratospheric ozone derived from merged SAGE II and Odin-OSIRIS satellite observations

... The SAGE II instrument, operational from 1984 to 2005, measured solar transmittance in the ultraviolet, visible and near infrared wavelength ranges in order to infer profiles of ... See full document

12

Toward a combined SAGE II-HALOE aerosol climatology: an evaluation of HALOE version 19 stratospheric aerosol extinction coefficient observations

Toward a combined SAGE II-HALOE aerosol climatology: an evaluation of HALOE version 19 stratospheric aerosol extinction coefficient observations

... 2.45 and 5.26 µm show similar behavior in the stratosphere as the channels at ...3.40 and 3.46 µm. An exception to this is that the minor erup- tions in the 2000s are not clearly detectable ... See full document

12

Comparison of aerosol extinction between lidar and SAGE II over Gadanki, a tropical station in India

Comparison of aerosol extinction between lidar and SAGE II over Gadanki, a tropical station in India

... clouds and aerosols from the troposphere to the strato- sphere since June 2006 and its measurements have provided a wealth of ...information. In Vernier et al. (2011a), observations ... See full document

12

Optimal estimation retrieval of aerosol microphysical properties from SAGE II satellite observations in the volcanically unperturbed lower stratosphere

Optimal estimation retrieval of aerosol microphysical properties from SAGE II satellite observations in the volcanically unperturbed lower stratosphere

... role in the climate system because they can influence the global chemical and radiation balance in the atmosphere in a num- ber of ways (McCormick et ...1999). In the aftermath of large ... See full document

23

Analysis of stratospheric NO<sub>2</sub> trends above Jungfraujoch using ground-based UV-visible, FTIR, and satellite nadir observations

Analysis of stratospheric NO<sub>2</sub> trends above Jungfraujoch using ground-based UV-visible, FTIR, and satellite nadir observations

... created from SAGE II, CALIPSO, and ENVISAT/GOMOS observational data ...changes in aerosol loading related to the Mount Pinatubo eruption as well as smaller changes due to a series of ... See full document

33

Evolution of stratospheric ozone and water vapour time series studied with satellite measurements

Evolution of stratospheric ozone and water vapour time series studied with satellite measurements

... SBUV and SBUV/2 (collec- tively referred to as ...Nimbus-7 satellite launched in October 1978, while more improved versions of the SBUV/2 were developed and placed aboard subsequent missions, ... See full document

21

Global cloud top height retrieval using SCIAMACHY limb spectra: model studies and first results

Global cloud top height retrieval using SCIAMACHY limb spectra: model studies and first results

... best observable for the SCIAMACHY tangent height at about 9 km. But there is also a higher percentage of MIPAS top heights that clearly lie outside the vertical field of view depicted by the dotted line. Most of these ... See full document

58

A study of polar ozone depletion based on sequential assimilation of satellite data from the ENVISAT/MIPAS and Odin/SMR instruments

A study of polar ozone depletion based on sequential assimilation of satellite data from the ENVISAT/MIPAS and Odin/SMR instruments

... with satellite data but individual satellite measure- ments are by and large more noisy which makes the method more difficult to ...implement. Ozone depletion is instead of- ten estimated by ... See full document

13

Sensitivity of polar stratospheric ozone loss to uncertainties in chemical reaction kinetics

Sensitivity of polar stratospheric ozone loss to uncertainties in chemical reaction kinetics

... through September. Varying the heterogeneous reaction rates by a factor of 2 changes the time of O 3 <0.1 ppmv by less than an hour. Heterogeneous reactions on liquid ternary solution droplets and the ... See full document

28

Limb–nadir matching using non-coincident NO&lt;sub&gt;2&lt;/sub&gt; observations: proof of
concept and the OMI-minus-OSIRIS prototype product

Limb–nadir matching using non-coincident NO<sub>2</sub> observations: proof of concept and the OMI-minus-OSIRIS prototype product

... the OSIRIS and OMI stratospheric VCDs for these latitudes and ...the OSIRIS and OMI stratospheres is very good given the rudimentary nature of the OMI SCD-bias cor- ...the ... See full document

20

Towards a merged satellite and in situ fluorescence ocean chlorophyll product

Towards a merged satellite and in situ fluorescence ocean chlorophyll product

... tology and the treatment of fluorescence data measured by a profiling ...verge in the future: at the present time, the only clima- tology available (Conkright et ...data and suffers from (1) a ... See full document

15

Towards a merged satellite and in situ fluorescence ocean chlorophyll product

Towards a merged satellite and in situ fluorescence ocean chlorophyll product

... color and induced fluorescence, see later), fluores- cence is undoubtedly the one which has been the least scientifically ...of in situ data, in terms of numbers of observations ...profiles ... See full document

41

Measurements of total and tropospheric ozone from IASI: comparison with correlative satellite, ground-based and ozonesonde observations

Measurements of total and tropospheric ozone from IASI: comparison with correlative satellite, ground-based and ozonesonde observations

... lower. In order to examine precisely the regions characterized by larger discrepancies, relative differences between IASI and GOME-2 total ozone columns have been calculated for each season ... See full document

17

Global distributions and trends of atmospheric ammonia (NH&lt;sub&gt;3&lt;/sub&gt;) from IASI satellite observations

Global distributions and trends of atmospheric ammonia (NH<sub>3</sub>) from IASI satellite observations

... Adon, M., Galy-Lacaux, C., Yoboué, V., Delon, C., Lacaux, J. P., Castera, P., Gardrat, E., Pien- aar, J., Al Ourabi, H., Laouali, D., Diop, B., Sigha-Nkamdjou, L., Akpo, A., Tathy, J. P., Lavenu, F., and Mougin, ... See full document

42

Characteristics of tropospheric ozone depletion events in the Arctic spring: analysis of the ARCTAS, ARCPAC, and ARCIONS measurements and satellite BrO observations

Characteristics of tropospheric ozone depletion events in the Arctic spring: analysis of the ARCTAS, ARCPAC, and ARCIONS measurements and satellite BrO observations

... Kalnay, E., Kanamitsu, M., Kistler, R., Collins, W., Deaven, D., Gandin, L., Iredell, M., Saha, S., White, G., Woollen, J., Zhu, Y., Chelliah, M., Ebisuzaki, W., Higgins, W., Janowiak, J., Mo, K. C., Ropelewski, C., ... See full document

39

Uncertainties in modelling the stratospheric warming following Mt. Pinatubo eruption

Uncertainties in modelling the stratospheric warming following Mt. Pinatubo eruption

... Hence, in the volcanic aerosol nucleation plume, the new volcanic aerosols formed after the eruption do not coagulate quickly and the relationship be- tween extinctions and effective radii breaks ... See full document

35

Combined assimilation of IASI and MLS observations to constrain tropospheric and stratospheric ozone in a global chemical transport model

Combined assimilation of IASI and MLS observations to constrain tropospheric and stratospheric ozone in a global chemical transport model

... layers and the continental surface in summer, which enhances the DFS and the number of pixels that pass the AVK trace filter ...3f and 4f), which depend mostly on the ocean–atmosphere thermal ... See full document

51

Formaldehyde production from isoprene oxidation across NO&lt;sub&gt;&lt;i&gt;x&lt;/i&gt;&lt;/sub&gt; regimes

Formaldehyde production from isoprene oxidation across NO<sub><i>x</i></sub> regimes

... J., and Hatch, C.: Instrumentation and Measurement Strategy for the NOAA SENEX Aircraft Campaign as Part of the Southeast Atmosphere Study 2013, ...doi:10.5194/amt-2015-388, in review, ... See full document

14

Chemical ozone loss in the Arctic winter 1991&amp;ndash;1992

Chemical ozone loss in the Arctic winter 1991&ndash;1992

... chemical ozone loss has occurred. Later in March and April, ER-2 aircraft observations are not considered, because they were taken far outside of the polar vortex (see ...HALOE ... See full document

33

Show all 10000 documents...