However/Therefore

• Hydrosphere: Long term climatic events can potentially lower the storage capacity significantly.
• Lithosphere: Processes such as surface runoff and precipitation input water into this store
• Atmosphere: Evaporation increases due to climate change can increase amount of water stored as gas (water vapour) in the atmosphere
• Atmosphere positive feedback: More condensation leads to more precipitation
• Atmosphere negative feedback: More precipitation increases the amount of water in the hydrosphere
• Cryosphere: Temprature increases due to global warming, which reduces the amount of water stored in the cryosphere, however increases the amount of water in the hydrosphere
• Water store inputs: precipitation, snow melt, groundwater flow , evapotranspiration
• Water store outputs: Evaporation, percolation, surface runoff