Provide several reasons for regional precipitation differences.

List two factors that will influence the movement of groundwater through sediments?

The information collected in St. Paul can be used to calculate the storage rate for each watershed, which is the difference between total input rates and total output rates: Storage Rate = Total Flux In Total Flux Out Q3.2. Use the information in the figure to fill out the table below. Enter a number into each box, then click "Check Answer" for feedback. Trout Brook Check Answer Total Flux In (Inputs) Total Flux Out (Outputs) - Storage Rate Rates for Nitrogen (kg ha-1 y-¹) 1 2 3 Note: To launch your computer's calculator, select Calculator from the CONTENTS menu (button in top left corner). For calculator help, click here. Deposition 14.5 N-Fixation 1.6 Pet Waste 5.9 Fertilizer 28.2 Compost 0.9 Nitrogen Budget Suburban Nitrogen Fluxes (kg ha-¹y-¹) Atmospheric Terrestrial Hydrologic E Denitrification 5.7 Street Sweeping 0.2 Yard Waste Removal 5.6 Storm Drain 9.9 Leaching to Groundwater 7.9 Nitrogen budget for the Trout Brook watershed in St. Paul. Adapted from Hobbie et al. (2017).

Please help with explanation

Given a FiO2 of 60% estimate the minimum acceptable PaO2 A) 150 mmHg B) 300 mmHg C) 109 mmHg D) 240 mmHg

Suggest some possible implications of the phenomenon shown in the table (e.g. for the fishing industry or drainage basin management). Explain why these interpretations are not as reliable as the data itself.