Land‐Atmosphere Responses to a Total Solar Eclipse in Three Ecosystems With Contrasting Structure and Physiology
Land‐Atmosphere Responses to a Total Solar Eclipse in Three Ecosystems With Contrasting Structure and Physiology
复制标题
具有对比结构和生理学的三个生态系统中的陆地-大气对日全食的响应
DOI:
10.1029/2018jd029630
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发表时间:
2019
期刊:
影响因子:
--
通讯作者:
Speck, A.
中科院分区:
文献类型:
--
作者:
Wood, J. D.;Sadler, E. J.;Fox, N. I.;Greer, S. T.;Gu, L.;Guinan, P. E.;Lupo, A. R.;Market, P. S.;Rochette, S. M.;Speck, A.
Mid‐Missouri experienced up to 2 min 40 s of totality at around solar noon during the total eclipse of 2017. We conducted the Mid‐Missouri Eclipse Meteorology Experiment to examine land‐atmosphere interactions during the eclipse. Here, research examining the eclipse responses in three contrasting ecosystems (forest, prairie, and soybeans) is described. There was variable cloudiness around first and fourth contacts (i.e., the start and end of partial solar obscuration) at the forest and prairie; however, solar irradiance (K↓) signals during the eclipse were relatively clean. Unfortunately, the eclipse forcing at the soybean field was contaminated by convective activity, which decreasedK↓beginning about an hour before first contact and exposed the field to cold outflow ~30 min before second contact. Turbulence was suppressed during the eclipse at all sites; however, there was also an amplified signal at the soybean field during the passage of a gust front. The standard deviations of the horizontal and vertical wind velocities and friction velocities decreased by ~75% at the forest (aerodynamically rough), and ~60% at the prairie (aerodynamically smooth). The eddy fluxes of energy were highly coherent with the solar forcing with the latent and sensible heat fluxes approaching 0 W/m2and changing in direction, respectively. For the prairie site, we estimated a canopy‐scale time constant for the surface conductance light response of 10 min. Although the eclipse imparted large forcings on surface energy balances, the air temperature response was relatively muted (1.5–2.5 °C decrease) due to the absence of topographic effects and the relatively moist land and atmosphere.
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DOI:
10.2307/1550088
发表时间:
1974
期刊:
Arctic and alpine research
影响因子:
--
作者:
R. Stewart;W. Rouse
通讯作者:
W. Rouse
影响因子:
6.2
作者:
R. Desjardins;D. Worth;E. Pattey;A. VanderZaag;R. Srinivasan;M. Mauder;D. Worthy;C. Sweeney;S. Metzger
通讯作者:
R. Desjardins;D. Worth;E. Pattey;A. VanderZaag;R. Srinivasan;M. Mauder;D. Worthy;C. Sweeney;S. Metzger
影响因子:
5.2
作者:
D. Turner;V. Wulfmeyer;A. Behrendt;T. Bonin;A. Choukulkar;R. Newsom;W. Brewer;D. Cook
通讯作者:
D. Cook
影响因子:
--
作者:
Bai Yang;P. Hanson;J. Riggs;S. Pallardy;M. Heuer;K. P. Hosman;T. Meyers;S. Wullschleger;L. Gu
通讯作者:
L. Gu
影响因子:
1.9
作者:
S. Burt
通讯作者:
S. Burt