Answer: A) greater than
Explanation:
Continental climates usually have a greater annual variation in temperature than coastal regions, meaning hot summers followed by cold winters. This happens because winds that blow overland prevail
in inland areas, and the temperatures are not decreased by nearby bodies of water. Coastal areas have a smaller range of temperature than continental land because of the ocean´s heat capacity.
Answer:
If lava cools slowly and does not move too fast it forms smooth ropy lava called pahoehoe.
However, if it cools quickly and moves fast it can tear into clinkery pieces called a'a
Answer:
The answer would be a theocracy
Here are some FUN FACTS to help expand your knowledge :)
Fun fact 1: In Greek Theocracy means "rule by gods"
Fun fact 2: This Government was first employed in the first Century A.D. by Josephus Flavius
Fun fact 3: This Government was mostly practiced by the jews
Fun fact 4: It was to be told that Moses ruled a theocracy
Fun fact 5: Islamic States, Holy See (Vatican City), Israel, and Central Tibetan Administration
Fun fact 6: Theocracy is a compound word for Theos (god) and Kratia (rule)
Fun fact 7: Some ancient time Theocracies are Pharaos, Babylonians, Assyrians, and Cretans.
Fun fact 8: There is a protected Theocracy at a place called Mount Athos.
Fun fact 9: In 2011 most Theocracies were ruled in islamic states
Answer: A - P.M. Grootes, K.M. Cuffey, and J.M. Bolzan, among others.
Explanation: Dr. Anandakrishnan collaborated and coauthored with all of the people listed above and has worked with many other people.
During the year 1994, Dr. Sridhar Anandakrishnan collaborated with Kurt M Cuffey, Richard B Alley, Pieter M Grootes and John M Bolzan on the topic 'Calibration of the δ18O isotopic paleothermometer for central Greenland, using borehole temperatures'
They calibrated the δ 18O paleo-thermometer for central Greenland using borehole temperatures, a thermal model forced by a measured δ 18O record and a formal inverse technique. The calibration is determined mostly by temperature fluctuations of the last several centuries, including the Little Ice Age.
Results are generally insensitive to model variables, including initial condition, basal boundary condition, parameterization of snow thermal properties, ice thickness and likely errors in temperature and isotope measurements. Results of this borehole calibration also seem to be in agreement with modern spatial gradients of δ 18O and temperature.
They suggest that calibrations of isotopic paleothermometers using borehole temperatures are a useful paleoclimate tool because they are independent of spatial gradients and include the effects of prehistoric temperatures.
