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						|  Climate Change Indicators: Stream 
					Temperature 
 This indicator shows changes in stream water temperature 
					across the Chesapeake Bay region.
 
 Key Points
 
 From 1960 through 2014, water temperature increased at 79 
					percent of the stream sites measured in the Chesapeake Bay 
					region (see Figure 1). More than half of these increases 
					were statistically significant. Only 5 percent of stations 
					had a significant temperature decrease over the same period.
 
 Since 1960, the Chesapeake Bay region has experienced an 
					overall increase in stream water temperature. Temperature 
					has risen by an average of 1.2°F across all sites and 2.2°F 
					at the sites where trends were statistically significant.
 
 Stream temperatures have risen throughout the Chesapeake Bay 
					region. The largest increases have occurred in the southern 
					part of the region.
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						| Background 
 Water temperature is an important physical property of every 
					river and stream. Many plants, animals, and other organisms 
					living in streams can flourish only in a specific range of 
					water temperatures. Temperature can affect certain aspects 
					of water quality. For example, higher temperatures reduce 
					levels of dissolved oxygen in the water, which can 
					negatively affect the growth and productivity of aquatic 
					life. Persistently warmer temperatures in streams can 
					accelerate natural chemical reactions and release excess 
					nutrients into the water. A stream’s water temperature can 
					also influence the circulation or mixing patterns in the 
					water it flows into, like bays and estuaries, potentially 
					affecting nutrient levels and salinity.
 
 Temperatures can vary naturally along the length of a 
					stream, from cold temperatures near a source of meltwater to 
					higher temperatures near its outlet to the sea. The 
					temperature at any given point is a product of many 
					different factors, including sources of water (for example, 
					melted snow, a recent rainstorm, or groundwater), the amount 
					of water in the stream (streamflow), air temperature, plants 
					along the bank (for example, trees that provide shade), and 
					the amount of development within the watershed. Over time, 
					however, an area’s climate has the strongest natural 
					influence on a stream’s temperature.
 
 The Chesapeake Bay is the largest estuary in the United 
					States, an important habitat for countless aquatic species, 
					and a driver of the regional economy. As rising air 
					temperatures (see the U.S. and Global Temperature indicator) 
					cause stream temperatures to rise, warmer stream water 
					coming into the bay can stress plants and animals and worsen 
					the effects of nutrient pollution that the bay is already 
					facing.
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						| About the Indicator 
 The U.S. Geological Survey maintains thousands of stream 
					gauges across the United States. Each gauge measures water 
					levels several times a day, typically every 15 minutes. 
					Field technicians visit each gauging station an average of 
					eight times a year to measure various stream conditions, 
					including water temperature. This indicator shows how 
					average water temperatures throughout the year changed 
					between 1960 and 2014 at 129 stream gauges located across 
					the Chesapeake Bay region. These stations were selected 
					because they had high-quality data for this entire time 
					period.
 
 Indicator Notes
 
 In addition to climate, changes to a stream’s average water 
					temperature can be influenced by other factors such as 
					industrial discharges, changes to local hydrology (such as 
					construction and operation of dams and channels), and 
					changes to land cover in the watershed. This indicator uses 
					measurements from all stream gauges with sufficient data. 
					Thus, it includes some stream sites that are likely more 
					disturbed by human activities than others. A more detailed 
					analysis of this data set found that water temperature tends 
					to increase more quickly than air temperature in 
					agricultural areas without major dams, but more slowly at 
					forested sites and in areas influenced by dams. Nonetheless, 
					a comparison of 35 relatively undisturbed reference stations 
					with the remaining 94 stations in this indicator showed no 
					significant difference in trends between the two groups of 
					stations.
 
 This indicator is based on measurements that are collected 
					an average of eight times per year, but more in some years 
					and less in others. The data were analyzed in a way that 
					accounts for variations in timing and makes it possible to 
					compare average temperatures across many years.
 
 Data Sources
 
 This indicator is based on an analysis developed by the U.S. 
					Geological Survey (USGS). Periodic temperature data were 
					collected by the USGS, and these data are stored in the USGS 
					National Water Information System.
 
 Technical Documentation
 
 Download related technical information PDF
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						|  Figure 
					1. Changes in Stream Water Temperatures in the 
					Chesapeake Bay Region, 1960–2014 This map shows the change in water temperature at 129 stream 
					gauges across the Chesapeake Bay region from 1960 to 2014. 
					Red circles show locations where temperatures have 
					increased; blue circles show locations where temperatures 
					have decreased. Filled circles represent sites where the 
					change was statistically significant.
 Data source: Jastram and Rice, 20153
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						| EPA Page |  
						| This is the
					
					EPA page for this topic. To see if the Trump 
					administration has changed the EPA page, simply click the 
					link and compare the information with this page. If you 
					notice changes were made to the EPA page, please post a 
					comment. Thanks. |  | 
			
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									| Additional Climate Change Information |  
									| Climate Change and Carbon Dioxide (Beginner - Listening, 
reading)
 
 A video lesson to 
		help with your understanding of climate change 
and carbon dioxide.
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 Great English listening and reading practice.
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									| Carbon Dioxide and Climate Change (Beginner - Listening, 
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 A video lesson to 
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 The English is 
		spoken at 75% of normal speed.
 Great English listening and reading practice.
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 Great English listening and reading practice.
 
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 A video lesson to 
		help with your understanding of climate change.
 The English is 
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 Great English listening and reading practice.
 
 A group of scientists say sea levels are rising at record rates. Another group 
found that January temperatures in the Arctic reached a record high.
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									| Capturing CO2 Gas Is Not Easy (Beginner - Listening, 
reading)
 
 A video lesson to 
		help with your understanding of climate change.
 The English is 
		spoken at 75% of normal speed.
 Great English listening and reading practice.
 
 Most scientists agree that carbon-dioxide gas is partly to blame for climate 
change: rising global temperatures. But capturing the CO2 gas released by power 
stations is costly and difficult.
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									| Growth, Climate Change Threaten African Plants and 
Animals (Beginner - Listening, 
reading)
 
 A video lesson to 
		help with your understanding of climate change.
 The English is 
		spoken at 75% of normal speed.
 Great English listening and reading practice.
 
 Researchers believe Africa may lose as much as 30 percent of its animal and 
plant species by the end of this century.
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