Skip to main content
Geosciences LibreTexts

7.9: Review and Additional Resources

  • Page ID
    21733
  • \( \newcommand{\vecs}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}} } \)

    \( \newcommand{\vecd}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash {#1}}} \)

    \( \newcommand{\id}{\mathrm{id}}\) \( \newcommand{\Span}{\mathrm{span}}\)

    ( \newcommand{\kernel}{\mathrm{null}\,}\) \( \newcommand{\range}{\mathrm{range}\,}\)

    \( \newcommand{\RealPart}{\mathrm{Re}}\) \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\)

    \( \newcommand{\Argument}{\mathrm{Arg}}\) \( \newcommand{\norm}[1]{\| #1 \|}\)

    \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\)

    \( \newcommand{\Span}{\mathrm{span}}\)

    \( \newcommand{\id}{\mathrm{id}}\)

    \( \newcommand{\Span}{\mathrm{span}}\)

    \( \newcommand{\kernel}{\mathrm{null}\,}\)

    \( \newcommand{\range}{\mathrm{range}\,}\)

    \( \newcommand{\RealPart}{\mathrm{Re}}\)

    \( \newcommand{\ImaginaryPart}{\mathrm{Im}}\)

    \( \newcommand{\Argument}{\mathrm{Arg}}\)

    \( \newcommand{\norm}[1]{\| #1 \|}\)

    \( \newcommand{\inner}[2]{\langle #1, #2 \rangle}\)

    \( \newcommand{\Span}{\mathrm{span}}\) \( \newcommand{\AA}{\unicode[.8,0]{x212B}}\)

    \( \newcommand{\vectorA}[1]{\vec{#1}}      % arrow\)

    \( \newcommand{\vectorAt}[1]{\vec{\text{#1}}}      % arrow\)

    \( \newcommand{\vectorB}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}} } \)

    \( \newcommand{\vectorC}[1]{\textbf{#1}} \)

    \( \newcommand{\vectorD}[1]{\overrightarrow{#1}} \)

    \( \newcommand{\vectorDt}[1]{\overrightarrow{\text{#1}}} \)

    \( \newcommand{\vectE}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash{\mathbf {#1}}}} \)

    \( \newcommand{\vecs}[1]{\overset { \scriptstyle \rightharpoonup} {\mathbf{#1}} } \)

    \( \newcommand{\vecd}[1]{\overset{-\!-\!\rightharpoonup}{\vphantom{a}\smash {#1}}} \)

    \(\newcommand{\avec}{\mathbf a}\) \(\newcommand{\bvec}{\mathbf b}\) \(\newcommand{\cvec}{\mathbf c}\) \(\newcommand{\dvec}{\mathbf d}\) \(\newcommand{\dtil}{\widetilde{\mathbf d}}\) \(\newcommand{\evec}{\mathbf e}\) \(\newcommand{\fvec}{\mathbf f}\) \(\newcommand{\nvec}{\mathbf n}\) \(\newcommand{\pvec}{\mathbf p}\) \(\newcommand{\qvec}{\mathbf q}\) \(\newcommand{\svec}{\mathbf s}\) \(\newcommand{\tvec}{\mathbf t}\) \(\newcommand{\uvec}{\mathbf u}\) \(\newcommand{\vvec}{\mathbf v}\) \(\newcommand{\wvec}{\mathbf w}\) \(\newcommand{\xvec}{\mathbf x}\) \(\newcommand{\yvec}{\mathbf y}\) \(\newcommand{\zvec}{\mathbf z}\) \(\newcommand{\rvec}{\mathbf r}\) \(\newcommand{\mvec}{\mathbf m}\) \(\newcommand{\zerovec}{\mathbf 0}\) \(\newcommand{\onevec}{\mathbf 1}\) \(\newcommand{\real}{\mathbb R}\) \(\newcommand{\twovec}[2]{\left[\begin{array}{r}#1 \\ #2 \end{array}\right]}\) \(\newcommand{\ctwovec}[2]{\left[\begin{array}{c}#1 \\ #2 \end{array}\right]}\) \(\newcommand{\threevec}[3]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \end{array}\right]}\) \(\newcommand{\cthreevec}[3]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \end{array}\right]}\) \(\newcommand{\fourvec}[4]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \\ #4 \end{array}\right]}\) \(\newcommand{\cfourvec}[4]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \\ #4 \end{array}\right]}\) \(\newcommand{\fivevec}[5]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \\ #4 \\ #5 \\ \end{array}\right]}\) \(\newcommand{\cfivevec}[5]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \\ #4 \\ #5 \\ \end{array}\right]}\) \(\newcommand{\mattwo}[4]{\left[\begin{array}{rr}#1 \amp #2 \\ #3 \amp #4 \\ \end{array}\right]}\) \(\newcommand{\laspan}[1]{\text{Span}\{#1\}}\) \(\newcommand{\bcal}{\cal B}\) \(\newcommand{\ccal}{\cal C}\) \(\newcommand{\scal}{\cal S}\) \(\newcommand{\wcal}{\cal W}\) \(\newcommand{\ecal}{\cal E}\) \(\newcommand{\coords}[2]{\left\{#1\right\}_{#2}}\) \(\newcommand{\gray}[1]{\color{gray}{#1}}\) \(\newcommand{\lgray}[1]{\color{lightgray}{#1}}\) \(\newcommand{\rank}{\operatorname{rank}}\) \(\newcommand{\row}{\text{Row}}\) \(\newcommand{\col}{\text{Col}}\) \(\renewcommand{\row}{\text{Row}}\) \(\newcommand{\nul}{\text{Nul}}\) \(\newcommand{\var}{\text{Var}}\) \(\newcommand{\corr}{\text{corr}}\) \(\newcommand{\len}[1]{\left|#1\right|}\) \(\newcommand{\bbar}{\overline{\bvec}}\) \(\newcommand{\bhat}{\widehat{\bvec}}\) \(\newcommand{\bperp}{\bvec^\perp}\) \(\newcommand{\xhat}{\widehat{\xvec}}\) \(\newcommand{\vhat}{\widehat{\vvec}}\) \(\newcommand{\uhat}{\widehat{\uvec}}\) \(\newcommand{\what}{\widehat{\wvec}}\) \(\newcommand{\Sighat}{\widehat{\Sigma}}\) \(\newcommand{\lt}{<}\) \(\newcommand{\gt}{>}\) \(\newcommand{\amp}{&}\) \(\definecolor{fillinmathshade}{gray}{0.9}\)

    Review

    Creosote bush
    Figure \(\PageIndex{1}\):

    Review and assess your learning. Start with the "Important Terms and Concepts" to ensure you know the terminology related to the topic of the chapter and concepts discussed. Move on to the "Review Questions" to answer critical thinking questions about concepts and processes discussed in the chapter. Finally, test your overall understanding by taking the "Self-assessment quiz".

    Important Terms and Concepts
    • Climatology
      the study of the long-term state of the atmosphere, or climate
    • climate
      the long-term state of the atmosphere
    • climate classification
      ways to organize the wealth of information about Earth's climate to bring order and understanding to it
    • empirical classification
      classification systems based on observable facts such as temperature and precipitation.
    • genetic classification
      classification systems based on the cause of the climate like solar radiation, air masses, pressure systems, etc.
    • applied classification
      classification systems created for a particular climate-associated problem
    • Koeppen Climate Classification
      an empirical system largely based on annual and monthly means of temperature and precipitation
    • Tropical rain forest Climate
      supports one of the most lush and diverse environments on Earth. Located near the equator, it is characterized by year-round warm temperatures and copious rainfall
    • Monsoon Climate
      abundant rainfall concentrated in the high-sun season, located near the equator with warm temperatures throughout the year
    • Wet/Dry Tropical Climate
      it supports a ground cover of drought resistant grasses with scattered trees, but not enough rainfall to make agriculture a viable, life sustaining activity.
    • Tropical Steppe Climate
      transitional climate between the tropical wet and tropical dry climates
    • Tropical Desert Climate
      an environment of extremes: it is the driest and hottest place on earth. Rainfall is sporadic and in some years no measurable precipitation falls at all.
    • Dry Summer Subtropical Climate
      also known as the "Mediterranean" climate, wet winter/dry summer seasonality
    • Humid Subtropical Climate
      found on the east coast of continents, instable air with moderate amounts of precipitation in most months of the year and subject to cold temperatures during the winter
    • Humid Continental Climate
      noted for its variable weather patterns related to cyclonic storms and its large temperature range due to its interior location in mid-latitude continents
    • Midlatitude Steppe Climate
      shares many of the same characteristics that the tropical steppe has. Both are semi-arid climates that are affected by their interior continental or leeward orographic position. However, the midlatitude steppe experiences larger temperature ranges and receives more total rainfall than the tropical steppe climate.
    • Midlatitude Desert Climate
      shares many of the same climatic characteristics as the tropical deserts, and for many of the same reasons. While the tropical desert climates are considered "hot" deserts following Köppen's classification (BWh), midlatitude deserts are "cold" deserts
    • Humid (Marine) West Coast Climate
      found on the west coast of midlatitude continents and is very humid through most of the year. Its geographic location places it in the path of westerly winds from the ocean that bring cloudy skies, much precipitation, and mild temperatures.
    • Subarctic Climate
      Bitterly cold winters and mild summers result in the largest annual temperature range of any climate on Earth.
    • Tundra Climate
      transitional climate between the Subarctic and Ice cap climates. It is a region of rolling to nearly level terrain almost entirely devoid of trees. Polar climates like the tundra are characterized by very cold temperatures and generally dry conditions. Temperatures never rise above 10o C (50oF) during the summer.
    • Ice Cap Climate
      experiences the coldest temperatures on earth. Located near the poles, this climate experiences bitterly cold temperatures throughout the year, especially during the long polar night. The resulting humidity levels are so low that precipitation amounts may be similar to most deserts.

    Additional Resources

    Use these resources to further explore the world of geography

    Multimedia

    "The Climate System" (Met Office)

    "USGS Public Lecture Series: Climate Change 101 (August 2009)

    Climate Connections: NPR series on global warming

    "Polar Warming" (PBS) News Hour with Jim Lehrer. November 11, 2004 report on the impact of global climate change on the Arctic.

    Climate Change Series - (WGBH Forum Network). Six part series includes topics of global climate change and the Arctic, The Southern Ocean, The Media, Ask the Experts, Northern Forests, The Ross Ice Shelf

    "Global Warming" (NPR) All things Considered Sept 11, 2003 segment about puzzling climate change data that suggests "global warming isn't following the rules". (5:07)

    "Climate Change" (NPR) May 2004 three-part series on climate change issues facing New York City.

    "What's Happening to Alaska's Glaciers? Their Dynamic Response to Changing Climate and Other Factors" Dr. Bruce Molina (USGS) Descriptive Flyer pdf.

    Visualization

    visualization_icon_tiny2.gif Interactive Climate Map - M. Ritter

    bullet Global Warming: Early Warning Signs

    Readings

    readings icon Paleoclimatology: An Introduction (NASA EOS)

    readings icon Global Warming and Global Climate Change (Carnegie Mellon University)

    readings icon Climate Clues in the Ice (NASA EOS)

    readings icon The Warming of the Earth: A beginner's guide to global warming. (Woods Hole Research Center)

    Web Sites

    web site icon National Climatic Data Center

    web site icon World Climate Data Centers


    7.9: Review and Additional Resources is shared under a CC BY-NC-SA 4.0 license and was authored, remixed, and/or curated by LibreTexts.