Evidence of lunar phase influence on global surface air temperature

Intraseasonal oscillations appearing in a newly available 20‐year record of satellite‐derived surface air temperature are composited with respect to the lunar phase. The daily surface air temperature is one of the geophysical fields derived from the TOVS data processed at the NASA Goddard Laboratory for Atmospheres. Polar regions exhibit strong lunar phase modulation with higher temperatures occurring near full moon and lower temperatures at new moon, in agreement with previous studies. The polar response to the apparent lunar forcing is most robust in winter when solar influence is at minimum. In addition, the response appears to be influenced by ENSO events. The highest mean temperature range between full moon and new moon in the region between 60° and 90° latitude was recorded in 1983, 1986/87, and 1990/91. Although the largest signal is in the polar regions, anomalies tend to progress equartoward in both hemispheres so that the warming in the tropics occurs at the time of the new moon.