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Understanding Land–Atmosphere–Climate Coupling from the Canadian Prairie Dataset

Atmospheric Research, Pittsford, VT 05763, USA
Agriculture and Agri-Food Canada, Ottawa, ON K1A0C6, Canada
Author to whom correspondence should be addressed.
Environments 2018, 5(12), 129;
Received: 7 November 2018 / Revised: 28 November 2018 / Accepted: 29 November 2018 / Published: 4 December 2018
Analysis of the hourly Canadian Prairie data for the past 60 years has transformed our quantitative understanding of land–atmosphere–cloud coupling. The key reason is that trained observers made hourly estimates of the opaque cloud fraction that obscures the sun, moon, or stars, following the same protocol for 60 years at all stations. These 24 daily estimates of opaque cloud data are of sufficient quality such that they can be calibrated against Baseline Surface Radiation Network data to yield the climatology of the daily short-wave, long-wave, and total cloud forcing (SWCF, LWCF and CF, respectively). This key radiative forcing has not been available previously for climate datasets. Net cloud radiative forcing changes sign from negative in the warm season, to positive in the cold season, when reflective snow reduces the negative SWCF below the positive LWCF. This in turn leads to a large climate discontinuity with snow cover, with a systematic cooling of 10 °C or more with snow cover. In addition, snow cover transforms the coupling between cloud cover and the diurnal range of temperature. In the warm season, maximum temperature increases with decreasing cloud, while minimum temperature barely changes; while in the cold season with snow cover, maximum temperature decreases with decreasing cloud, and minimum temperature decreases even more. In the warm season, the diurnal ranges of temperature, relative humidity, equivalent potential temperature, and the pressure height of the lifting condensation level are all tightly coupled to the opaque cloud cover. Given over 600 station-years of hourly data, we are able to extract, perhaps for the first time, the coupling between the cloud forcing and the warm season imbalance of the diurnal cycle, which changes monotonically from a warming and drying under clear skies to a cooling and moistening under cloudy skies with precipitation. Because we have the daily cloud radiative forcing, which is large, we are able to show that the memory of water storage anomalies, from precipitation and the snowpack, goes back many months. The spring climatology shows the memory of snowfall back through the entire winter, and the memory in summer, goes back to the months of snowmelt. Lagged precipitation anomalies modify the thermodynamic coupling of the diurnal cycle to the cloud forcing, and shift the diurnal cycle of the mixing ratio, which has a double peak. The seasonal extraction of the surface total water storage is a large damping of the interannual variability of precipitation anomalies in the growing season. The large land-use change from summer fallow to intensive cropping, which peaked in the early 1990s, has led to a coupled climate response that has cooled and moistened the growing season, lowering cloud-base, increasing equivalent potential temperature, and increasing precipitation. We show a simplified energy balance of the Prairies during the growing season, and its dependence on reflective cloud. View Full-Text
Keywords: climate; land–atmosphere interaction; clouds; diurnal cycle; snow cover; Prairies; land-use; hydrometeorology climate; land–atmosphere interaction; clouds; diurnal cycle; snow cover; Prairies; land-use; hydrometeorology
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MDPI and ACS Style

Betts, A.K.; Desjardins, R.L. Understanding Land–Atmosphere–Climate Coupling from the Canadian Prairie Dataset. Environments 2018, 5, 129.

AMA Style

Betts AK, Desjardins RL. Understanding Land–Atmosphere–Climate Coupling from the Canadian Prairie Dataset. Environments. 2018; 5(12):129.

Chicago/Turabian Style

Betts, Alan K., and Raymond L. Desjardins 2018. "Understanding Land–Atmosphere–Climate Coupling from the Canadian Prairie Dataset" Environments 5, no. 12: 129.

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