Not exact matches
Keeping
heat at medium - high, cook fish on 1 side about 3 minutes (more or
less,
depending on size of fillets), until deep brown and crispy.
Remove from
heat and add tea bags, allowing them to steep for 5 - 10 minutes (more or
less depending on desired strength.)
--
Depending on how much
heat you like, you can use more or
less jalapeno in the dressing....
Bring the mixture to a boil; then reduce the
heat and simmer until it reduces in volume by half or
less (
depending on preference).
Directions: Use a broad bottomed pan for faster cooking / Dissolve the salt in the water / Add cornmeal gradually, whisking or stirring vigorously as you do so / On medium
heat, stir more or
less continuously until liquid comes to a simmer and begins to thicken / Turn
heat to low and, using a large spoon, continue to cook and give a thorough stir every minute or so / Polenta will continue to thicken and eventually begin to stick to itself, rather than to the pot / 15 — 25 minutes for cooking
depending on size of pot and type of cornmeal.
Fork the pickled onions and jalapeños on top, adding more or
less jalapeño
depending on your affinity for
heat.
Add the meatballs to the pan and cook over medium
heat for about 7 - 8 minutes, flipping after about 4 minutes (may take a little more or
less time
depending on size of meatballs).
grated fresh ginger 1 fresh green chili pepper, seeds removed, finely chopped 1 cup chopped spinach (I used frozen) 2 tablespoons ghee 1/4 teaspoon cumin seed or ground cumin (I used ground cumin but would try cumin seeds next time) 1/4 teaspoon crushed red pepper flakes (more or
less depending on your spicy
heat tolerance) 1 - 2 teaspoons lemon juice
Toss 3/4 cup Silver Swan soy sauce (or any kind, but this was what my family uses — it's made in the Philippines — and it adds a slightly sweeter flavor), 1 cup rice vinegar, 15 garlic cloves, 2 tablespoons black peppercorns, 3 bay leaves, 3 Thai chiles (more or
less depending on your
heat sensitivity), 2 tablespoons palm sugar (if you can't find it at the store, sugar in the raw will work), and a 2 - inch piece of ginger with 8 chicken drumsticks in a plastic bag and marinate — no bowl or pan washing required.
1 cup coconut milk 1 salmon fillet, weighing about 1 1/4 -1 1/2 pounds 3 tablespoons fish sauce 2 kaffir lime leaves 2 limes 3 - 4 bird's eye chilies (more or
less depending on your
heat tolerance)
The chipotles do have a bit of
heat, so
depending on your tolerance / preferences you may want to adjust more or
less...
--
Depending on how much
heat you like, you can use more or
less jalapeno in the dressing....
1 pound organic chicken breast, cut into small chunks 1 small onion, chopped 3 large carrots, chopped 2 cups shredded chard or other greens 1 bunch green onions, chopped 1 lemon or lime, juiced 1/2 cup cilantro, chopped 1 tablespoon chopped garlic 1 tablespoon chopped ginger 1/2 tablespoon of red pepper flakes (more or
less depending on your
heat tolerance) 1 can organic coconut milk 1 quart organic chicken broth sea salt to taste
Depending on income and current liabilities, with applications of
less than 20 % down, our lenders will use a conservative qualifying ratio of 35/42 %, whereby up to 35 % of your income is to be used towards the mortgage payment,
heating costs, property taxes and / or strata fee payments.
Usually a female dog would have gone through her first
heat at about 6 - 8 months more or
less depending on the breed.
Before allowing the temperature to respond, we can consider the forcing at the tropopause (TRPP) and at TOA, both reductions in net upward fluxes (though at TOA, the net upward LW flux is simply the OLR); my point is that even without direct solar
heating above the tropopause, the forcing at TOA can be
less than the forcing at TRPP (as explained in detail for CO2 in my 348, but in general, it is possible to bring the net upward flux at TRPP toward zero but even with saturation at TOA, the nonzero skin temperature requires some nonzero net upward flux to remain — now it just
depends on what the net fluxes were before we made the changes, and whether the proportionality of forcings at TRPP and TOA is similar if the effect has not approached saturation at TRPP); the forcing at TRPP is the forcing on the surface + troposphere, which they must warm up to balance, while the forcing difference between TOA and TRPP is the forcing on the stratosphere; if the forcing at TRPP is larger than at TOA, the stratosphere must cool, reducing outward fluxes from the stratosphere by the same total amount as the difference in forcings between TRPP and TOA.
Re my 414,413 PS the TOA forcing would be negative initially; after stratospheric adjustment it would be
less negative — it could be positive, but that
depends on the distribution of solar
heating
PS the TOA forcing would be negative initially; after stratospheric adjustment it would be
less negative — it could be positive, but that
depends on the distribution of solar
heating.
The net effect of the water vapor (more or
less heating) is not determinant and may be either positive or negative
depending on all the above.
The physical size of this large
heat storage
depends on the maximum temperature that the storage can be raised to — higher temperatures store more
heat in
less space.
Warmer winters (if they have lots of clouds... in winter thick clouds actually warm since there is
less daylight and there cooling effect is now reversed to warming by retaining the
heat... reflecting more IR than carbon dioxide can do,
depending upon the type of cloud).
Meaning twice the CO2 concentration could only absorb ~ 100 % of the energy in 5m instead of 10m, no more or
less heat is preserved in the atmosphere,
depending on CO2.
There would therefore be
heat moved from the equator (where the hot air rises) towards the poles (where it cools and becomes
less dense)-- errr,
depending on the shape of the planet.
An increase of solar radiation will lead to a rising temperature, to an extent
depending on the amount of ice on the surface; an ice cover will reflect much of the extra radiation away, causing
less heating, until eventually the
heating is sufficient to melt the ice.
Because this new technology can block both NIR light and visible light, occupants would have the ability to customize their climate
depending on whether they wanted more or
less visible light and more or
less heat.
Weatherstripping is an easy and cost - effective way to help your tenants spend
less energy and money
heating or cooling their house
depending on the season.