There are a diverse range of biological and geochemical signatures that can be interpreted as direct or indirect indicators
of hydrological change.
How important are differences between land cover reconstructions for our understanding
of hydrological change?
How important are current differences between land cover reconstructions for our understanding
of hydrological change?
Wetherald and Manabe (2002) provide a good description of the mechanism
of hydrological change simulated by GCMs.
When comparing the history
of hydrological changes in the region with artifacts from the Middle Stone Age, the researchers discovered a «striking correspondence between the archaeological record of South Africa and the timing of the abrupt climate change» as seen in the marine core, the study states.
http://www.springerlink.com/content/lm0024kv72t3841w/ «The simulated magnitude
of hydrological changes over land are much larger when compared to changes over oceans in the recent marine cloud albedo enhancement study since the radiative forcing over land needed (− 8.2 W m − 2) to counter global mean radiative forcing from a doubling of CO2 (3.3 W m − 2) is approximately twice the forcing needed over the oceans (− 4.2 W m − 2).
Not exact matches
2.6 the
change in the health
of the asset (s) expected if environmental water is not provided including with regard to the long - term environmental water requirements
of the asset (s) relative to recent
hydrological conditions; and
Taking factors such as sea surface temperature, greenhouse gases and natural aerosol particles into consideration, the researchers determined that
changes in the concentration
of black carbon could be the primary driving force behind the observed alterations to the
hydrological cycle in the region.
«Looking at
changes in the number
of dry days per year is a new way
of understanding how climate
change will affect us that goes beyond just annual or seasonal mean precipitation
changes, and allows us to better adapt to and mitigate the impacts
of local
hydrological changes,» said Polade, a postdoctoral researcher who works with Scripps climate scientists Dan Cayan, David Pierce, Alexander Gershunov, and Michael Dettinger, who are co-authors
of the study.
The paradox is that this season stands in such stark contrast to the past 11 years
of drought, highlighting the types
of variability that climate
change can wreak on the
hydrological cycle.
New data show that extreme weather events have become more frequent over the past 36 years, with a significant uptick in floods and other
hydrological events compared even with five years ago, according to a new publication, «Extreme weather events in Europe: Preparing for climate
change adaptation: an update on EASAC's 2013 study» by the European Academies» Science Advisory Council (EASAC), a body made up
of 27 national science academies in the European Union, Norway, and Switzerland.
Co-author Dr Alison Kay from the Centre for Ecology & Hydrology said: «Our
hydrological modelling suggests that the increased likelihood
of extreme rainfall arising from human - made climate
change gives a more modest increase in extreme flows in the River Thames.
January 2004: «Directions for Climate Research» Here, ExxonMobil outlines areas where it deemed more research was necessary, such as «natural climate variability, ocean currents and heat transfer, the
hydrological cycle, and the ability
of climate models to predict
changes on a regional and local scale.»
Studies
of climate
change using global climate models with a focus on
changes in the
hydrological cycle.
For the
hydrological modelling
of the Thames river catchment done at CEH we showed that the
changes in atmospheric circulation and precipitation caused higher peak 30 - day river flow, while flood risk mapping revealed a small increase in flood risk for properties in the Thames catchment.
Conversion to arable land
changes the
hydrological regime In the present study, the cause for the decrease in species diversity is the
changing hydrological regime resulting from the conversion
of forest to arable land.
These
changes made China a unique region to investigate the impact
of aerosols on regional climate and the
hydrological cycle.
It has been argued that the land amplification is associated with lapse rate
changes (not represented in the UVic model), and it is certain that drying
of the land can play a role (not reliable in the UVic model since diffusing water vapor gives you a crummy
hydrological cycle, especially over land).
Because meter - scale suboxic zones occur today within the mobile mud belts
of tropical river - dominated continental shelves, such as the Amazon Shelf, we hypothesize that sedimentological and
hydrological changes during the PETM fostered the development
of analogous conditions on the Eastern seaboard
of North America.
The prize is awarded for «ground - breaking work that provides a powerful estimate
of the effects
of climate
change on the global
hydrological cycle, with a clear explanation
of the global water budget.»
The patterns
of salinity
change can be used to infer
changes in the Earth's
hydrological cycle over the oceans (Wong et al., 1999; Curry et al., 2003) and are an important complement to atmospheric measurements.
In the context
of future
changes in the atmospheric
hydrological cycle, understanding precipitation
changes in the subtropics is
of particular importance given
While the pupils above were making important
changes to the benefit
of their personal and social development, they and their class mates were also learning about rivers and the
hydrological cycle, co-operative working, and many other things that supported the work
of the class teacher.
Changes in ocean salinity can be a useful indicator of chagnes in the hydrological cycle, since the ocean integrates those c
Changes in ocean salinity can be a useful indicator
of chagnes in the
hydrological cycle, since the ocean integrates those
changeschanges.
As an integrating measurement made with high accuracy, freshwater content (salinity anomaly over a layer) is the most sensitive yardstick available for observing the global fingerprint
of a
changing hydrological cycle.
In many regions,
changing precipitation or melting snow and ice are altering
hydrological systems, affecting water resources in terms
of quantity and quality (medium confidence).
Global warming is one kind
of climate
change caused by an increased greenhouse effect with an impact on both meteorology and the
hydrological cycle.
Andy (or anyone else with full access)-- The abstract states that «Inferences from the observational record... indicate that models underestimate some
of the
changes in the
hydrological cycle.»
I know in general terms that the
hydrological cycle should intensify with warming and that one event is hard to pin on climate
change, but it would be good to do a catch up on how the broad trend
of extreme weather fits the models.
One
of the topics on my perpetually growing reading list will be the
changing energetics
of the
changing hydrological cycle.
The global map
of the A1B 2080 to 2099
change in annual mean precipitation is shown in Figure 10.12, along with other
hydrological quantities from the multi-model ensemble.
Visible
changes in
hydrological cycle have been observed in the form
of changing precipitation patterns, cropping patterns, droughts, water availability periods, frequency and intensity
of heatwaves, precipitation events and weather - induced natural disasters.
We need to look at the evaporative / condensation process combined with ALL aspects
of global weather as an ever
changing global heat energy removal system and not just as a part
of the
hydrological cycle as usually set out in models and schematic diagrams.
The end
of the first half
of the Holocene — between about 5 and 4 ka — was punctuated by rapid events at various latitudes, such as an abrupt increase in NH sea ice cover (Jennings et al., 2001); a decrease in Greenland deuterium excess, reflecting a
change in the
hydrological cycle (Masson - Delmotte et al., 2005b); abrupt cooling events in European climate (Seppa and Birks, 2001; Lauritzen, 2003); widespread North American drought for centuries (Booth et al., 2005); and
changes in South American climate (Marchant and Hooghiemstra, 2004).
Oxygen - isotope (λ 18O) evidence
of Holocene
hydrological changes at Signy Island, maritime Antarctica Noon, P.E., Leng, M.J. and Jones, V.J. 2003; The Holocene 13: 251 - 263
Relatively rapid degradation
of ice - rich permafrost is adversely affecting human infrastructure, altering Arctic ecosystem structure and function,
changing the surface energy balance, and has the potential to dramatically impact Arctic
hydrological process and increase greenhouse gas emissions.
Detection
of change in world - wide
hydrological time series
of maximum annual flow: report by a team
of experts under the leadership
of Zbigniew W. Kundzewicz.
with increasing stress on crops due to
changes in the
hydrological cycle and heat stress, more and more farmers are seeking answers from modified crops to heartier breeds
of cattle that are more accustomed to drought conditions such as those that come from Africa and India.
Development, use and application
of the HYDROSPECT data analysis system for the detection
of changes in
hydrological time series for use in WCP - Water and National Hydrological Services: report by Maciej Radzeijewski and Zbigniew W.
hydrological time series for use in WCP - Water and National
Hydrological Services: report by Maciej Radzeijewski and Zbigniew W.
Hydrological Services: report by Maciej Radzeijewski and Zbigniew W. Kundzewicz.
A survey
of current approaches to modelling
of hydrological time - series with respect to climate variability and
change by George S. Cavadias; prepared for the World Climate Program - Water, Project A2.
Changes in
hydrological cycles have taken place and the depletion
of water resources are the top challenges Nepal faces in context
of climate
change.
Wrona, F. J., et al. (2016), Transitions in Arctic ecosystems: Ecological implications
of a
changing hydrological regime, J. Geophys.
Surface movement,
hydrological change and equilibrium flow
of Lemon CreekGlacier, Alaska, J. Glaciol., 5 (37), 61 - 75.
This policy document consists
of a COP 16 position paper presenting the role that the weather, climate and
hydrological communities can play in effectively addressing the objectives
of the United Nations Framework Convention on Climate
Change (UNFCCC).
Contribution from working group I to the fifth assessment report by IPCC TS.5.4.1 Projected Near - term
Changes in Climate Projections
of near - term climate show small sensitivity to Green House Gas scenarios compared to model spread, but substantial sensitivity to uncertainties in aerosol emissions, especially on regional scales and for
hydrological cycle variables.
Degradation
of near - surface permafrost (perennially frozen ground) caused by modern climate
change is adversely affecting human infrastructure, altering Arctic ecosystem structure and function,
changing the surface energy balance, and has the potential to dramatically impact Arctic
hydrological processes and increase greenhouse gas emissions.
Instead, the speed
of the
hydrological cycle
changes to a miniscule extent in order to maintain sea surface and surface air temperature equilibrium.
The Swedish Meteorological and
Hydrological Institute (SMHI) presents unique data which depict regional climate
change after a rise in global temperature
of 1.5 degrees.
This technical document includes the analysis and findings
of an on - line survey on the role
of National Meteorological and
Hydrological Services (NMHSs) in adaptation to climate variability and
change.
These stationary - wave
changes lead to large regional
changes in the
hydrological cycle and modify the sensitivity
of the
hydrological cycle to global warming.