Representativeness of CO and O3 Along ATom Transects Derived from GEOS-5 and GMI-CTM Simulations

Liu, Junhua ; Strode, Sarah A ; Prather, Michael J ; Lait, Leslie R ; Conaty, Austin ; Damon, Megan ; Steenrod, Stephen ; Newman, Paul A ; Commane, Roisin ; Daube, Bruce(Harvard Univ, Cambridge, MA, United States)

关键词: ATMOSPHERIC CHEMISTRY;    ATMOSPHERIC MODELS;    ATLANTIC OCEAN;    CARBON MONOXIDE;    GEOS SATELLITES (ESA);    GPM SATELLITE CONSTELLATION;    HETEROGENEITY;    OZONE;    PACIFIC OCEAN;    PROBABILITY DENSITY FUNCTIONS;    SIMULATION;    TOMOGRAPHY;    VARIABILITY;   

RP-ID  :  GSFC-E-DAA-TN67698

学科分类：地质物理学

美国|英语

来源: NASA Technical Reports Server

【 摘 要 】

One major goal for the NASA Atmospheric Tomography Mission (ATom) is producing an observation-based chemical climatology to represent the atmospheric heterogeneity. In this study, we use CO and O3 observations and global atmospheric model simulations to examine the spatial representativeness of the ATom-1 and -2 transects within a 4D framework provided by the NASA GEOS-5 and GMI-CTM models. Based on the probability density functions, we find that the variability of CO and O3 along the flight tracks is well hindcast by the model when sampled per ATom flights. The CO variations along the ATom-transect are likely representative of the typical CO variations over the whole Pacific basin during both the ATom-1 and -2 periods, the northern Atlantic during the ATom-1 period, and the tropical Atlantic in the ATom-2 period. Over southern Atlantic, CO along the ATom-1 transects is likely less well mixed than that of the broader region, but is still representative of the median CO concentration. CO along the ATom-2 transect is likely higher than the median CO concentration over this region. For O3, the agreements between PDFs of O3 sampled along the ATom transects and over the broader regions are fair to good over all six regions (Scores > 0.65) with notable discrepancies over some regions. For example, in ATom-1 over the northern Pacific and Atlantic, the transect samples air masses with higher O3 levels. During ATom-2, the transect over-represents the occurrence of O3 plumes over tropical Pacific. Over the southern Pacific and Atlantic for both ATom-1 and -2, the transects have a less uniform distribution compared to the surrounding basins, but still represent the median O3 abundance. Overall, we conclude in most cases that ATom measurements represent the statistical variations of these two species over the ocean basins at the time of measurement. Higher-order statistics, including covariance of species, has not been tested in this study.