Earth's Mesosphere During Possible Encounters With Massive Interstellar Clouds 2 and 7 Million Years Ago

Author:

Miller Jesse A.12ORCID,Opher Merav12ORCID,Hatzaki Maria3ORCID,Papachristopoulou Kyriakoula34ORCID,Thomas Brian C.5ORCID

Affiliation:

1. Department of Astronomy Boston University Boston MA USA

2. SHIELD NASA DRIVE Center Boston MA USA

3. Section of Geography and Climatology Department of Geology and Geoenvironment National and Kapodistrian University of Athens Athens Greece

4. Institute for Astronomy Astrophysics Space Applications and Remote Sensing National Observatory of Athens (IAASARS/NOA) Athens Greece

5. Department of Physics and Astronomy Washburn University Topeka KS USA

Abstract

AbstractOur solar system's path has recently been shown to potentially intersect dense interstellar clouds 2 and 7 million years ago: the Local Lynx of Cold Cloud and the edge of the Local Bubble. These clouds compressed the heliosphere, directly exposing Earth to the interstellar medium. Previous studies that examined climate effects of these encounters argued for an induced ice age due to the formation of global noctilucent clouds (NLCs). Here, we revisit such studies with a modern 2D atmospheric chemistry model using parameters of global heliospheric magnetohydrodynamic models as input. We show that NLCs remain confined to polar latitudes and short seasonal lifetimes during these dense cloud crossings lasting ∼105 years. Polar mesospheric ozone becomes significantly depleted, but the total ozone column broadly increases. Furthermore, we show that the densest NLCs lessen the amount of sunlight reaching the surface instantaneously by up to 7% while halving outgoing longwave radiation.

Funder

Heliophysics Division

Publisher

American Geophysical Union (AGU)

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