The phrase "average annual surface" is not entirely clear and may not be correct in written English without additional context.
It could be used in contexts discussing climate data, environmental studies, or geographical measurements, but it needs clarification.
Example: "The average annual surface temperature in this region has increased over the past decade."
Alternatives: "mean yearly surface" or "typical annual surface".
For perspective if one is needed, the average annual surface flow of the Indus is ten times as much as the flow of the Colorado River.
Figure 3 shows a map of modern average annual surface ocean temperatures for the Atlantic Ocean. Figure 5 shows species' abundances in surface sediments at the ocean bottom as a percent of all the planktonic foraminifera there.
The average annual surface runoff varied from 379 to 386 mm while the evapotranspiration of the village was in the range of 359 364 mm.
Table 3 Average annual surface water inflow upstream (based on 20 years data) River or stream Average annual flow (million m3) Tukituki 126.9 Waipawa 264.1 Avoca 9.4 Tukipo 11.6 Mangatewai 27.8 Makaretu 40.9 Porangahau 12.9 Maharakeke 10.3 Total 503.9.
These values are only slightly above the average annual surface temperature of Muscat (29 °C), and significantly lower than peak temperatures during summer time (47 °C) and therefore constitute a suitable target for rejecting process waste heat.
We used our water withdrawal and consumption maps in conjunction with the average annual surface and ground freshwater availability to compute both indicators.
Decrease in mean annual surface temperature averaged over all irrigated grid cells is rather small (~0.04 K or ~1.2%), but the changes are particularly pronounced in the highly irrigated areas [Fig. 5; data source: Siebert et al. (2015)] and during the growing seasons.
Lal and Singh (2001) and Lal (2001) have reported that the average annual mean surface temperature over Indian sub-continent is likely to increase by about 2.7 and 3.8 °C during the decades of 2050 and 2080 s, respectively.
The average total annual surface water outflow at W6 and T6 is ~725 million m3.
Linearising carbon fluxes [ 5] and neglecting difference between the changes of globally averaged annual mean surface air and sea surface temperatures one obtains (5) F X c p l = β X d q CO 2 c p l / d t + γ X d T g c p l / d t, F X u c p l = β X d q CO 2 u c p l / d t, where X = l, oc, T g stands for globally averaged annual mean temperature, and γ X and β X were defined in Introduction.
The model produces digital maps of long-term average, seasonal and annual surface runoff, evapotranspiration and groundwater recharge.
