Search Results - "Daleu, C. L."

  • Showing 1 - 5 results of 5
Refine Results
  1. 1

    Characterizing Convection Schemes Using Their Responses to Imposed Tendency Perturbations by Hwong, Y. L., Song, S., Sherwood, S. C., Stirling, A. J., Rio, C., Roehrig, R., Daleu, C. L., Plant, R. S., Fuchs, D., Maher, P., Touzé‐Peiffer, L.

    “…Convection is usually parameterized in global climate models, and there are often large discrepancies between results obtained with different convection…”
    Get full text
    Journal Article
  2. 2

    Intercomparison of methods of coupling between convection and large‐scale circulation: 1. Comparison over uniform surface conditions by Daleu, C. L., Plant, R. S., Woolnough, S. J., Sessions, S., Herman, M. J., Sobel, A., Wang, S., Kim, D., Cheng, A., Bellon, G., Peyrille, P., Ferry, F., Siebesma, P., van Ulft, L.

    “…As part of an international intercomparison project, a set of single‐column models (SCMs) and cloud‐resolving models (CRMs) are run under the weak‐temperature…”
    Get full text
    Journal Article
  3. 3

    Memory Properties in Cloud‐Resolving Simulations of the Diurnal Cycle of Deep Convection by Daleu, C. L., Plant, R. S., Woolnough, S. J., Stirling, A. J., Harvey, N. J.

    “…A series of high‐resolution three‐dimensional simulations of the diurnal cycle of deep convection over land are performed using the new Met Office NERC…”
    Get full text
    Journal Article
  4. 4

    Intercomparison of methods of coupling between convection and large‐scale circulation: 2. Comparison over nonuniform surface conditions by Daleu, C. L., Plant, R. S., Woolnough, S. J., Sessions, S., Herman, M. J., Sobel, A., Wang, S., Kim, D., Cheng, A., Bellon, G., Peyrille, P., Ferry, F., Siebesma, P., van Ulft, L.

    “…As part of an international intercomparison project, the weak temperature gradient (WTG) and damped gravity wave (DGW) methods are used to parameterize…”
    Get full text
    Journal Article
  5. 5

    Using the Weak‐Temperature Gradient Approximation to Evaluate Parameterizations: An Example of the Transition From Suppressed to Active Convection by Daleu, C. L., Plant, R. S., Woolnough, S. J.

    “…Two single‐column models are fully coupled via the weak‐temperature gradient approach. The coupled‐SCM is used to simulate the transition from suppressed to…”
    Get full text
    Journal Article