Validation of stratospheric nitric acid profiles observed by Improved Limb Atmospheric Spectrometer (ILAS)–II

[1] The Improved Limb Atmospheric Spectrometer-II (ILAS-II) was launched aboard the Advanced Earth Observing Satellite-II (ADEOS-II) in December 2002. Stratospheric vertical profiles of nitric acid (HNO3) concentration observed by ILAS-II (version 1.4) are validated using coincident HNO3 measurements by balloon-borne instruments (MIPAS-B2 and MkIV) in March and April 2003. Further validation is performed by making climatological comparisons of lower stratospheric HNO3-ozone (O3) correlations obtained by ILAS-II and ILAS (the predecessor of ILAS-II) for specific potential vorticity-based equivalent latitudes and seasons where and when ILAS data showed very compact correlations in 1997. The reduced scatter of ILAS-II HNO3 values around the reference HNO3, which is derived from ILAS-II O3 using the ILAS HNO3-O3 correlation, shows that the precision of the ILAS-II HNO3 data is better than 13–14%, 5%, and 1% at 15, 20, and 25 km, respectively. Combining all of the comparisons made in the present study, the accuracy of the ILAS-II HNO3 profiles at 15–25 km is estimated to be better than −13%/+26%.

[1]  L. Froidevaux,et al.  Interhemispheric Differences in Polar Stratospheric HNO3, H2O, CIO, and O3 , 1995, Science.

[2]  D. Weisenstein,et al.  In situ observations of NOy, O3, and the NOy/O3 ratio in the lower stratosphere , 1996 .

[3]  Guido Maucher,et al.  Design and characterization of the balloon-borne Michelson Interferometer for Passive Atmospheric Sounding (MIPAS-B2). , 2004, Applied optics.

[4]  G. Manney,et al.  Correlations of stratospheric abundances of NO y , O3, N2O, and CH4 derived from ATMOS measurements , 1998 .

[5]  D. Fahey,et al.  Reactive nitrogen and its correlation with ozone in the lower stratosphere and upper troposphere , 1993 .

[6]  Tatsuya Yokota,et al.  Tangent height registration for the solar occultation satellite sensor ILAS: A new technique for Version 5.20 products , 2002 .

[7]  Ellis E. Remsberg,et al.  The Area of the Stratospheric Polar Vortex as a Diagnostic for Tracer Transport on an Isentropic Surface , 1986 .

[8]  H. Irie,et al.  Investigation of polar stratospheric cloud solid particle formation mechanisms using ILAS and AVHRR observations in the Arctic , 2004 .

[9]  William G. Read,et al.  Three‐dimensional structure and evolution of stratospheric HNO3 based on UARS Microwave Limb Sounder measurements , 2004 .

[10]  F. Goutail,et al.  Ozone profiles in the high‐latitude stratosphere and lower mesosphere measured by the Improved Limb Atmospheric Spectrometer (ILAS)‐II: Comparison with other satellite sensors and ozonesondes , 2006 .

[11]  Tatsuya Yokota,et al.  Arctic polar stratospheric clouds observed with the Improved Limb Atmospheric Spectrometer during winter 1996/1997 , 2000 .

[12]  Malcolm K. W. Ko,et al.  Interrelationships between mixing ratios of long‐lived stratospheric constituents , 1992 .

[13]  Laurence S. Rothman,et al.  The HITRAN molecular spectroscopic database: edition of 2000 including updates through 2001 , 2003 .

[14]  Tatsuya Yokota,et al.  Improved Limb Atmospheric Spectrometer (ILAS) data retrieval algorithm for Version 5.20 gas profile products , 2002 .

[15]  Wesley A. Traub,et al.  Validation of CFC‐12 measurements from the Improved Limb Atmospheric Spectrometer (ILAS) with the version 6.0 retrieval algorithm , 2002 .

[16]  H. L. Miller,et al.  On the relationship between stratospheric aerosols and nitrogen dioxide , 1993 .

[17]  M. Santee,et al.  A Lagrangian approach to studying Arctic polar stratospheric clouds using UARS MLS HNO3 and POAM II aerosol extinction measurements , 2002 .

[18]  Y. Kondo,et al.  Denitrification and nitrification in the Arctic stratosphere during the winter of 1996–1997 , 2000 .

[19]  K. Jucks,et al.  A comparison of Arctic HNO3 profiles measured by the Improved Limb Atmospheric Spectrometer and balloon‐borne sensors , 2000 .

[20]  Tatsuya Yokota,et al.  Improved Limb Atmospheric Spectrometer (ILAS) for stratospheric ozone layer measurements by solar occultation technique , 1999 .

[21]  H. Nakajima,et al.  A Lagrangian method to study stratospheric nitric acid variations in the polar regions as measured by the Improved Limb Atmospheric Spectrometer , 2003 .

[22]  M. Santee,et al.  UARS Microwave Limb Sounder observations of denitrification and ozone loss in the 2000 Arctic late winter , 2000 .

[23]  L. Froidevaux,et al.  MLS observations of ClO and HNO3 in the 1996–97 Arctic Polar Vortex , 1997 .

[24]  S. R. Kawa,et al.  Partitioning of reactive nitrogen in the midlatitude lower stratosphere , 2000 .

[25]  P. Newman,et al.  An objective determination of the polar vortex using Ertel's potential vorticity , 1996 .

[26]  Y. Kondo,et al.  Evidence for the nucleation of polar stratospheric clouds inside liquid particles , 2003 .

[27]  G. Toon The JPL MkIV interferometer , 1991 .

[28]  Y. Sasano,et al.  Characteristics of Arctic polar stratospheric clouds in the winter of 1996/1997 inferred from ILAS measurements , 2002 .

[29]  R. McKenzie,et al.  Impact of Pinatubo aerosols in the partitioning between NO and HNO , 1994 .

[30]  K. Jucks,et al.  Validation of ozone measurements from the Improved Limb Atmospheric Spectrometer , 2002 .

[31]  D. Fahey,et al.  Photochemical partitioning of the reactive nitrogen and chlorine reservoirs in the high-latitude stratosphere , 1992 .

[32]  L. Froidevaux,et al.  Six years of UARS Microwave Limb Sounder HNO3 observations: Seasonal, interhemispheric, and interannual variations in the lower stratosphere , 1999 .

[33]  Y. Sasano,et al.  Redistribution of nitric acid in the Arctic lower stratosphere during the winter of 1996–1997 , 2001 .

[34]  Gerald Wetzel,et al.  NOy partitioning and budget and its correlation with N2O in the Arctic vortex and in summer midlatitudes in 1997 , 2002 .

[35]  G. Toon,et al.  Measurements of reactive nitrogen in the stratosphere , 1998 .

[36]  L. Froidevaux,et al.  UARS Microwave Limb Sounder HNO3 observations: Implications for Antarctic polar stratospheric clouds , 1998 .