Bromwich, D.H., F.M. Robasky, R.I. Cullather, and M.L. Van Woert, 1995:
The atmospheric hydrologic cycle over the Southern Ocean and Antarctica from operational numerical analyses.
Not exact matches
Predicting how increasing
atmospheric CO2 will affect the
hydrologic cycle, from extreme weather forecasts to long - term projections on agriculture and water resources, is critical both to daily life and to the future of the planet.
The basic principle is that the
hydrologic cycle accelerates — warming enhances evaporation, increases
atmospheric water content, and subsequently enhances precipitation as well
Note also that there appears — already started — to be a likely increase in drought frequency with
atmospheric warming and associated acceleration of the
hydrologic cycle, assuming continued greenhouse gas emissions.
If so, I think we want to include tightly coupled chemical and biological processes, in that case — for example, the chemical fate of
atmospheric methane over time, the effects of increasing
atmospheric CO2 on oceanic acid - base chemistry, and the response of the biological components of the carbon
cycle to increased temperatures and a changing
hydrologic cycle.
Hydrologic cycle; moisture transport and air - ground exchange; water budgets of meteorological phenomena; climatology of
atmospheric water
As an academic and
hydrologic forecaster, I have followed an energy centric, reproducible data path to quantify correlations between solar
cycles and
atmospheric moisture patterns.
Dr Lenton (who is also one of the creators of the planetary - boundaries concept) and Dr Watson suggest that energy might be used to change the
hydrologic cycle with massive desalination equipment, or to speed up the carbon
cycle by drawing down
atmospheric carbon dioxide, or to drive new recycling systems devoted to tin and copper and the many other metals as vital to industrial life as carbon and nitrogen are to living tissue.
Chapter 13: Variability and change in the
atmospheric branch of the Arctic
hydrologic cycle.
Absorbing aerosols heat the air, alter regional
atmospheric stability and vertical motions, and affect the large - scale circulation and
hydrologic cycle with significant regional climate effects.
Regarding the
hydrologic cycle, multiple factors operate, including important changes in
atmospheric circulation patterns, as Chris Colose mentioned.
Do we really have the understanding and sensitivity in all of our measuring to capture the energy budget as it changes form, phase, and location, or are there possibly slow changes in thermocline depths,
hydrologic cycle speeds,
atmospheric elevations, large ocean currents etc, that can receive energy quickly but manifest it as temperature slowly or even imperceptibly in regard to our ability to capture these changes?