Growing Season Air mass Equivalent Temperature (T_E) in the East Central USA

Authors

Dolly Na-Yemeh, University of Oklahoma, NormanFollow
Rezaul Mahmood, University of Nebraska-LincolnFollow
Gregory Goodrich, Western Kentucky UniversityFollow
Keri Younger, Western Kentucky UniversityFollow
Kevin Cary, Western Kentucky UniversityFollow
Joshua D. Durkee, Western Kentucky UniversityFollow

Document Type

Article

Date of this Version

8-19-2020

Citation

Climate 2020, 8, 95;

doi:10.3390/cli8090095

Comments

© 2020 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license

Abstract

Equivalent temperature (T_E), which incorporates both dry (surface air temperature, T) and moist heat content associated with atmospheric moisture, is a better indicator of overall atmospheric heat content compared to T alone. This paper investigates the impacts of different types of air masses on T_E during the growing season (April–September). The study used data from the Kentucky Mesonet for this purpose. The growing season was divided into early (April–May), mid (June–July), and late (August–September). Analysis suggests that T_E for moist tropical (MT) air mass was as high as 61 and 81 °C for the early and mid-growing season, respectively. Further analysis suggests that T_E for different parts of the growing seasons were statistically significantly different from each other. In addition, T_E for different air masses was also statistically significantly different from each other. The difference between T_E and T (i.e. T_E-T) is smaller under dry atmospheric conditions but larger under moist conditions. For example, in Barren County, the lowest difference (20–10 °C) was 10 °C. It was reported on 18 April 2010, a dry weather day. On the other hand, the highest difference for this site was 48 °C and was reported on 11 August 2010, a humid day.