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Projected future climate: Difference between revisions

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==Relevance==
==Relevance==


Continued warming of the basin’s climate will further impact the surface water balance and hydrology, leading to chronic drought conditions by today's standards in the absence of a large increase in average precipitation. More warming will also further stress the basin’s ecosystems and species, potentially beyond thresholds for viability in some cases.
Continued warming of the basin’s climate will further impact the surface water balance and hydrology, leading to chronic drought conditions by today's standards in the absence of a large increase in average precipitation. More warming will also further stress the basin’s ecosystems and species, potentially beyond thresholds for viability in some cases.  
 
==Methods==
 
===Global climate models===
 
===Downscaling===


==Future temperature==
==Future temperature==
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==Drought indicators==
==Drought indicators==


==Other climate metrics=
==Other climate metrics==


==Data and tools==
==Data and tools==

Revision as of 17:29, 11 May 2021

Overview

Figure 1. Annually averaged temperature over the Colorado River Basin, 1895-2020, shown with the blue and red bars as anomalies from a late 20th- century (1971-2000) baseline. The gray line is a 10-year running average plotted on the 6th year, and the. The dashed yellow line is the linear trend from 1980-2020, showing 2.1°F of warming over that period. (Design: Jeff Lukas, updated from Lukas and Payton 2020, based on gridded climate data from NOAA NCEI Climate-at-a-Glance; https://www.ncdc.noaa.gov/cag/.)

As described in Recent climate change, the climate of the Colorado River Basin has become substantially warmer in the past 40 years, very likely due to human changes to the atmosphere and climate system. Meanwhile, average precipitation in the basin has not clearly changed, but the underlying atmospheric processes (e.g., circulation patterns, water vapor content) are already being influenced by the warming global climate.

Both basic physics and our most sophisticated tools (global climate models; GCMs) tell us that further warming will occur in the basin over at least the next several decades, at a similar or greater rate than what has been observed since 1980. Neither the physics nor the GCMs present a clear picture of future precipitation change, however.

Relevance

Continued warming of the basin’s climate will further impact the surface water balance and hydrology, leading to chronic drought conditions by today's standards in the absence of a large increase in average precipitation. More warming will also further stress the basin’s ecosystems and species, potentially beyond thresholds for viability in some cases.

Methods

Global climate models

Downscaling

Future temperature

Figure 2. Fraction of the area of the Southwest U.S. (UT, CO, AZ, NM) experiencing extremely warm (upper 10%; red bars) and extremely cool (lower 10%; blue bars) daily high temperatures averaged over the summer (June-August), 1895-2020. Note the abrupt increase in the area experiencing extremely warm summer daily highs after 1995. The green line is a 9-point smoothing filter to emphasize decadal-scale variability. (Chart: NOAA NCEI https://www.ncdc.noaa.gov/extremes/cei/; annotation on y-axis by Jeff Lukas)



Future precipitation

As discussed in Climate patterns and variability, annual precipitation in the basin is highly variable, and there are no recent trends in annual or seasonal precipitation that clearly emerge from the background “noise” of historical year-to-year and decadal variability, as with temperature. But the most recent two decades does stand out for overall dryness, which is accentuated by the preceding two wet decades in the 1980s and 1990s (Figures 3 & 4). By slight margins, 2000-2020 has been the driest 21-year period on record in both the Upper Basin (with 94% of the 20th-century average) and Lower Basin (88% of the 20th-century average). The period since 2000 also includes the driest single water years on record in the Upper Basin (2018) and Lower Basin (2002).

Figure 3. Upper Colorado River Basin water-year precipitation, 1900-2020 (green dots and line), with smoothing filter that emphasizes multi-year variability (dark red line). (NOAA NCEI Climate-at-a-Glance; https://www.ncdc.noaa.gov/cag/)
Figure 4. Lower Colorado River Basin water-year precipitation, 1900-2020 (green dots and line), with smoothing filter that emphasizes multi-year variability (dark red line). (NOAA NCEI Climate-at-a-Glance; https://www.ncdc.noaa.gov/cag/)


Drought indicators

Other climate metrics

Data and tools

There are several climate tools that are useful for plotting and examining time-series and recent trends in temperature, precipitation, and other climate variables over specific areas (states, counties, river basins, etc.). Each tool depicts one or more Gridded climate datasets (LINK), so it is advised that users of the tools familiarize themselves with these datasets as well.

NOAA NCEI Climate at a Glance - Regional Time Series

The “CAG” tool is a versatile tool that can be used to generate many types of charts, maps, and analyses from NOAA’s official nClimGrid monthly gridded climate dataset. The link above opens the Regional and Time Series options, allowing users to plot temperature, precipitation, and other variables for the Upper Basin, Lower Basin, or many other U.S. basins and regions. All variables can be plotted from 1895 to present.


Additional resources

State of the Science Report

Chapter 2 of the State of the Science report describes recent climate changes in greater detail, in section 2.10.

NCA4 Climate Science Special Report

The 2018 Climate Science Special Report (CSSR), Volume 1 of the Fourth National Climate Assessment (NCA4), describes the historical record and likely causes of recent temperature change (Ch 6.1, 6.2) and recent precipitation change (Ch. 7.1) in the U.S.

Research directions

New and Notable Research (2020-present)

[<URL FOR PAPER>]

Summary