The news comes as one important atmospheric measuring station at Cape Grim in Australia is poised on the verge of 400ppm for the first time.
Besides spending three decades developing the capability to model future climates, the CSIRO has, for decades, been key in running one of only three "baseline" atmospheric measuring stations, at Cape Grim in Tasmania.
Winds over the past couple of months have gone back and forth from looking favorable to unfavorable to El Niño development, and the Southern Oscillation Index, an atmospheric measure, has stayed on the neutral side of the El Niño threshold.
Due to the absence of long-term, high-resolution atmospheric measure ments in the Cordillera Blanca, however, longer-term, process-based assessments of the glacier-atmosphere link (e.g., Mölg et al. 2009) is problematic.
The intra-abdominal pressure (IAP) was measured continuously with a pressure transducer calibrated to atmospheric pressure measured at the mid-thoracic level.
Extended Data Fig. 3 Atmospheric transmittances measured by NOMAD during the storm.
In January, the next frontier of atmospheric CO2 measuring instruments will begin when the National Aeronautics and Space Administration launches the first carbon-scanning satellite, called the Orbiting Carbon Observatory.
Local radioactive fallout is confirmed by the total beta activity of daily atmospheric precipitation measured at regional weather stations.
In this short paper we examine the possible connection between atmospheric parameters measured at low and middle altitudes and geomagnetic storms occurred in 2000 and 2003.
Fig. 6 Atmospheric temperatures measured by the microlimb sounder onboard the AURA satellite (AURA/MLS version 3.3 data) at an altitude of 0.046 hPa (~86 km) above 48°N, 145°E (the NLC region in the event).
The ZHD is due to the mix of dry gases in the atmosphere and can be modeled by means of consolidated relations involving the latitude and height of the GNSS station and atmospheric pressure measured in its proximity.
